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"","Serial","Continent","Region.Plate","Country","State..or.the.like.","Source.General","Source.Common.Name","Obsidian.Age","Secondary.Age","Ages.Average","Formation.Type","Boundary.Activity","Boundary.Type","Crust.Type","Normative.Occurrence","Latitude","Longitude","Loc..Notes","Conservative.Grouping","Hypothetical.Grouping","Tool.Quality","Type","Geology","Ethnominerology","Other.Names","Bibliographies","Known.","Catalogued.","X","Total.No..Known","Total.No..Catalogued","Total..","X.1","X.2","X.3","X.4","X.5","X.6","X.7","X.8","X.9","X.10","X.11","X.12","X.13","MeanNa","MeanMg","MeanK","MeanSc","MeanTi","MeanMn","MeanFe","MeanCo","MeanZn","MeanGa","MeanRb","MeanSr","MeanY","MeanZr","MeanNb","MeanSb","MeanCs","MeanBa","MeanLa","MeanCe","MeanNd","MeanTb","MeanDy","MeanSm","MeanEu","MeanYb","MeanLu","MeanHf","MeanTa","MeanPb","MeanTh","MeanU","SDNa","SDMg","SDK","SDSc","SDTi","SDMn","SDFe","SDCo","SDZn","SDGa","SDRb","SDSr","SDY","SDZr","SDNb","SDSb","SDCs","SDBa","SDLa","SDCe","SDNd","SDTb","SDDy","SDSm","SDEu","SDYb","SDLu","SDHf","SDTa","SDPb","SDTh","SDU","n"
"KEN019","KEN019","Africa","African Rift","Kenya","Bomet","Kibikoni","Kibikoni Group General","","",NA,"","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.817,35.301,"","Southern Kenya Rift Valley","","","Obsidian","""There are two subsources for this glass (Brown et al 2013).""","","""Literature suggests alternate names for this source include: Lake Naivasha (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,57790.2871894159,NA,36277.1794980679,NA,NA,2168.46260114466,0,NA,NA,NA,149,5,174,1286,309,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9168.10903942573,NA,4548.89121171394,NA,NA,184.26767674371,0,NA,NA,NA,14.4047204210393,1.06834549089184,21.4994300971056,146.92889551955,43.1045085212443,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"KEN055","KEN055","Africa","African Rift","Kenya","Meru","Mackinder Valley","Mackinder Valley 1","","",NA,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.105,37.293,"","Mount Kenya","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,79452.371732817,NA,45242.706696675,NA,NA,2168.46260114466,46021.6795040391,NA,NA,NA,138,214,43,1076,315,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12604.6787948973,NA,5673.10231209174,NA,NA,184.26767674371,7079.07048033131,NA,NA,NA,13.3412846852579,45.7251870101708,5.31307755273298,122.935841041241,43.9414892692296,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"KEN056","KEN056","Africa","African Rift","Kenya","Meru","Mackinder Valley","Mackinder Valley 2","","",NA,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.116,37.294,"","Mount Kenya","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,80490.9648273637,NA,45491.7491188586,NA,NA,2245.90769404268,41685.2902498591,NA,NA,NA,163,136,43,1374,360,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12769.4458379678,NA,5704.33039821336,NA,NA,190.848665198842,6412.04560224538,NA,NA,NA,15.7581840847611,29.0589973522581,5.31307755273298,156.983127872366,50.2188448791196,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"KEN057","KEN057","Africa","African Rift","Kenya","Meru","Mackinder Valley","Mackinder Valley 3","","",NA,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.116,37.294,"","Mount Kenya","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,81381.1874798322,NA,46404.9046668648,NA,NA,2323.35278694071,44482.9607364268,NA,NA,NA,155,330,53,1280,313,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12910.6747320283,NA,5818.83338065923,NA,NA,197.429653653975,6842.38423326855,NA,NA,NA,14.9847762769201,70.5108023988616,6.54867698360112,146.243379677313,43.6624956865678,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"KEN059","KEN059","Africa","African Rift","Kenya","Turkana","North Island","North Island 1","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.068,36.044,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,43917.6508551146,NA,33205.6562911376,NA,NA,22381.6318475288,41125.7561525456,NA,NA,NA,133.5,90,68,779,302,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6967.29210698337,NA,4163.74481621412,NA,NA,30009.5487960824,6325.97787604075,NA,NA,NA,2.12132034355964,7.07106781186548,25.4558441227157,29.698484809835,1.4142135623731,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"KEN060","KEN060","Africa","African Rift","Kenya","Turkana","North Island","North Island 2","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.068,36.044,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31520.1528094956,NA,NA,NA,NA,125,15,94,708,308,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2678.46230123893,NA,NA,NA,NA,12.0844969975162,3.20503647267553,11.6146346501605,80.8908693840137,42.9650117299134,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN061","KEN061","Africa","African Rift","Kenya","Turkana","North Island","North Island 3","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.068,36.044,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34617.9565254166,NA,NA,NA,NA,116,11,80,657,309,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2941.70183944424,NA,NA,NA,NA,11.214413213695,2.35036007996205,9.88479544694508,75.0639847249958,43.1045085212443,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN062","KEN062","Africa","African Rift","Kenya","Turkana","North Island","North Island 4","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.068,36.044,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,52817.5533564521,NA,NA,NA,NA,148,81,94,809,307,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4488.23412640037,NA,NA,NA,NA,14.3080444450592,17.3071969524478,11.6146346501605,92.4303860616767,42.8255149385825,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN065","KEN065","Africa","African Rift","Kenya","Turkana","North Island","North Island Group General","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.068,36.044,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ndiema, K E, C. D. Dillian, D. R. Braun, J. W. K. Harris, and P. W. Kiura. Transport and Subsistence Patterns in the Transition to Pastoralism, Koobi Fora, Kenya. Archaeometry 53, 6 (2011) 1085-1098. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2646.7517,847.8234,38150.6917,NA,163.8423,NA,127.0541,72.6853,87.1702,127.8789,746.2165,NA,NA,660.6199,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,759.578822512267,228.677208091425,6393.69454920473,NA,28.1381072847245,NA,12.9485757213336,44.8958752301119,4.86794160925448,16.5967076885749,52.5278413103206,NA,NA,349.843900149274,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10
"KEN066","KEN066","Africa","African Rift","Kenya","Nakura","Broad Acres","Broad Acres 1","","0.002",0.002,"Pyroclastic Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.858,36.362,"","Ol Karia/South Lake Naivasha","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,41321.168118748,NA,37024.3067646184,NA,NA,309.780371592095,209.825286492579,NA,321,NA,408,NA,207,1419,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6555.37449930698,NA,4642.57547007874,NA,NA,26.3239538205301,32.2753973267384,NA,47.4433819564741,NA,39.4437981998928,NA,25.5769082189704,162.124496689146,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN067","KEN067","Africa","African Rift","Kenya","Nakuru","Broad Acres","Broad Acres 2","","0.002",0.002,"Pyroclastic Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.86,36.362,"","Ol Karia/South Lake Naivasha","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,41662.4201355276,NA,36559.4275765425,NA,NA,464.670557388142,69.9417621641931,NA,314.4,NA,394.2,NA,218.6,1408.6,243,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1071.97002658832,NA,302.745640032033,NA,NA,6.35528743231302e-14,10.7584657755795,NA,10.3101891350256,NA,13.718600511714,NA,5.94138031100518,30.2539253651489,80.541914553852,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"KEN069","KEN069","Africa","African Rift","Kenya","Bomet","Kibikoni","Kibikoni 1","","0.002",0.002,"Pyroclastic Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.817,35.301,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Lake Naivasha (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,39724.0459081093,NA,38478.650653139,NA,NA,390.948786264061,4.7076186072053,NA,284.80612244898,NA,404.769230769231,1,203.25,2007.98076923077,489.08,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,557.853465301234,NA,852.962080379569,NA,NA,29.774922832027,26.4271624410921,NA,25.9223000996845,NA,9.96866410746538,0.213669098178368,9.48191142327622,38.7861988061489,146.459510688042,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,104
"KEN070","KEN070","Africa","African Rift","Kenya","Bomet","Kibikoni","Kibikoni 2","","0.002",0.002,"Pyroclastic Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.817,35.301,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Lake Naivasha (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,41061.5198451114,NA,36899.7855535266,NA,NA,425.94801093913,69.9417621641931,NA,295.5,NA,399,2,220,1478.5,325,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1521.24931295542,NA,410.899032901222,NA,NA,54.7619503578149,10.7584657755795,NA,9.19238815542512,NA,1.4142135623731,0.427338196356737,1.4142135623731,13.4350288425444,45.3364571825385,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"KEN073","KEN073","Africa","African Rift","Kenya","Marsabit","Ndiema Suregei","Ndiema Suregei Source 2","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.391,36.471,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,619.560743184189,34970.8810820966,NA,NA,NA,164,20,138,1285,303,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,52.6479076410601,5379.23288778975,NA,NA,NA,15.8548600607412,4.27338196356737,17.0512721459803,146.814642879177,42.267527773259,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN074","KEN074","Africa","African Rift","Kenya","Marsabit","Ndiema Suregei","Ndiema Suregei Source 3","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.391,36.471,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,619.560743184189,41965.0572985159,NA,NA,NA,156,16,129,1304,289,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,52.6479076410601,6455.0794653477,NA,NA,NA,15.0814522529002,3.4187055708539,15.9392326581989,148.985443046263,40.3145726946265,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN075","KEN075","Africa","African Rift","Kenya","Marsabit","Ndiema Suregei","Ndiema Suregei Source 4","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.391,36.471,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7279.83873241422,41965.0572985159,NA,NA,NA,146,37,136,1231,298,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,618.612914782456,6455.0794653477,NA,NA,NA,14.1146924930989,7.90575663259963,16.8041522598066,140.645000299041,41.5700438166045,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN076","KEN076","Africa","African Rift","Kenya","Marsabit","Ndiema Suregei","Ndiema Suregei Source 5","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.391,36.471,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2400.79787983873,48959.2335149352,NA,NA,NA,139,35,137,1324,287,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,204.010642109108,7530.92604290565,NA,NA,NA,13.437960661238,7.4784184362429,16.9277122028935,151.270495853721,40.0355791119648,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN077","KEN077","Africa","African Rift","Kenya","Marsabit","Ndiema Suregei","Ndiema Suregei Source 6","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.391,36.471,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,851.89602187826,69242.3445425512,NA,NA,NA,126,25,142,1171,292,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,72.3908730064576,10650.8811178237,NA,NA,NA,12.1811729734963,5.34172745445921,17.5455119183275,133.789841876667,40.7330630686192,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN082","KEN082","Africa","African Rift","Kenya","Turkana","Southern Suguta","Southern Suguta 1","","0.0038",0.0038,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",1.532,36.264,"","","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36721.6844143272,NA,40759.9430973714,NA,NA,1781.23713665454,40286.4550065752,NA,NA,NA,214,6,128,1832,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5825.69187999453,NA,5110.99676190283,NA,NA,151.362734468047,6196.87628673378,NA,NA,NA,20.6886588597477,1.28201458907021,15.8156727151121,209.310837163154,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,261
"KEN083","KEN083","Africa","African Rift","Kenya","Turkana","Southern Suguta","Southern Suguta 2","","0.0038",0.0038,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",1.532,36.264,"","","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,49110.6163278477,NA,39431.7168457259,NA,NA,3020.35862302292,67563.7422506106,NA,NA,NA,143,1,89,1025,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7791.12732233612,NA,4944.44696925427,NA,NA,256.658549750168,10392.6779392098,NA,NA,NA,13.8246645651585,0.213669098178368,10.9968349347264,117.108956382223,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4
"KEN084","KEN084","Africa","African Rift","Kenya","Turkana","Suguta Waterfall","Suguta Waterfall 1","","0.0038",0.0038,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",1.476,36.215,"","","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,50965.2468538238,NA,34367.8542613274,NA,NA,2942.9135301249,76935.9383806124,NA,NA,NA,239,10,206,2408,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,8085.3541849621,NA,4309.47588478161,NA,NA,250.077561295036,11834.3123531374,NA,NA,NA,23.1055582592509,2.13669098178368,25.4533482758836,275.120358017945,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"KEN085","KEN085","Africa","African Rift","Kenya","Turkana","Suguta Waterfall","Suguta Waterfall 2","","0.0038",0.0038,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",1.476,36.215,"","","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,60386.7699257825,NA,36111.1512166122,NA,NA,3407.58408751304,72739.4326507608,NA,NA,NA,348,15,330,3912,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9580.02664710211,NA,4528.07248763286,NA,NA,289.56349202583,11188.8044066027,NA,NA,NA,33.6432396410851,3.20503647267553,40.7747812186485,446.956329138788,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"KEN086","KEN086","Africa","African Rift","Kenya","Turkana","Suguta Waterfall","Suguta Waterfall 3","","0.0038",0.0038,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",1.476,36.215,"","","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,41341.0420824663,NA,NA,2788.02334432885,65115.7805748638,NA,NA,NA,174,1,115,1381,287,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5183.86229618658,NA,NA,236.91558438477,10016.1316370645,NA,NA,NA,16.8216198205425,0.213669098178368,14.2093934549836,157.782896354976,40.0355791119648,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4
"KEN087","KEN087","Africa","African Rift","Kenya","Marsabit","Ndiema Suregei","Ndiema Suregei Group General","","0.001",0.001,"Tuff Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",4.391,36.471,"","Asille","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ndiema, K E, C. D. Dillian, D. R. Braun, J. W. K. Harris, and P. W. Kiura. Transport and Subsistence Patterns in the Transition to Pastoralism, Koobi Fora, Kenya. Archaeometry 53, 6 (2011) 1085-1098. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1686.26014285714,1660.56721428571,43848.2494285714,NA,271.482571428571,NA,146.9355,27.5332142857143,135.905642857143,154.021571428571,1224.90914285714,NA,NA,102.462615384615,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,338.008835498732,2292.48085793952,29194.8810497441,NA,16.8853131617814,NA,15.3635882965586,8.92837339978196,8.34395180868839,7.07040531657552,59.4243069806612,NA,NA,135.039002584154,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,14
"KEN088","KEN088","Africa","African Rift","Kenya","Nakuru","Suswa","Suswa Group General","","2.6",2.6,"Shield","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-1.099,36.45,"","Southern Kenya Rift Valley","East Rift","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Brown, F H, B.P. Nash, D.P. Fernandez, H.V. Merrick, and R.J. Thomas. Geochemical Composition of Source Obsidians from Kenya. Journal of Archaeological Science 40 (2013) 3233-3251. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,66880.1586849648,NA,42188.2746363652,NA,NA,65673.438777524,2777.09938004884,NA,NA,NA,187.147058823529,4,106.147058823529,1200.70588235294,215,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,524.568728605278,NA,880.497927645523,NA,NA,5580.67820995237,98.912588628871,NA,NA,NA,0.707106781186548,0.854676392713474,0.707106781186548,1.4142135623731,29.9918101361409,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34
"TNZ004","TNZ004","Africa","African Rift","Tanzania","Kilimanjaro","Mt. Kilimanjaro","Mt. Kilimanjaro Group General","","2.6-0",1.3,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-3.055,37.397,"","Kilimanjaro","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. An Energy-Dispersive X-Ray Fluorescence Analysis of Obsidian Artifacts from Tanzania, and One Kilimanjaro Source Sample. Archaeological Research Facility, UC Berkeley, 2012. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,584,142,3913,NA,21,NA,20,38,50,153,44,NA,NA,92,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,11,40,NA,NA,NA,NA,NA,8,4,5,NA,6,NA,4,5,6.17799715434068,3,8,NA,NA,6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.75202688824192,4.44366162977988,NA,1
"ARM001","ARM001","Eurasia","Persian Belt","Armenia","Shirak","Akhurian","Akhurian 1","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",40.579,43.704,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Akhurian River (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,572,622,6557,NA,64.2,NA,136,6.3,33.4,138,27.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10.7670172890245,52.8551863767844,1008.59998243781,NA,9.48867639129482,NA,13.1479327332976,1.34611531852372,4.12690209909957,15.7668643714603,3.86406111986559,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"ARM002","ARM002","Eurasia","Persian Belt","Armenia","Shirk","Akhurian","Akhurian 2","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",40.579,43.704,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Akhurian River (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,492,NA,7361,NA,NA,NA,134,1.8,35.5,161,26.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9.26114074510502,NA,1132.27153739892,NA,NA,NA,12.9545807813373,0.384604376721063,4.38637797958188,18.394675100037,3.7245643285347,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"ARM003","ARM003","Eurasia","Persian Belt","Armenia","Aragatsotn","Arteni","Arteni 1","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",40.32,43.98,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Arteni A, Mez Arteni, Aragatz, Talin (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., G. Bigazzi, Y. Keheyan, S. Meloni. Characterization of Armenian Obsidians: Implications for Raw Material Supply for Prehistoric Artifacts. Journal of Radioanalytical and Nuclear Chemistry, Vol 243, No 3 (2000) 673-682. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,341,701,3377,NA,41.7,NA,145,8.5,24.2,45,39.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6.41879876845694,59.5683049037393,519.451294905061,NA,6.16320569341112,NA,14.0180165171188,1.81618733451613,2.99015062270089,5.14136881678053,5.53802261583624,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"ARM004","ARM004","Eurasia","Persian Belt","Armenia","Aragatsotn","Arteni","Arteni 2","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",40.32,43.98,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Arteni B, Mez Arteni , Talin (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., G. Bigazzi, Y. Keheyan, S. Meloni. Characterization of Armenian Obsidians: Implications for Raw Material Supply for Prehistoric Artifacts. Journal of Radioanalytical and Nuclear Chemistry, Vol 243, No 3 (2000) 673-682. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,449,568,3837,NA,44.5,NA,129,15,17.3,49.9,29.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,8.45173210274828,48.2664724469671,590.20865222112,NA,6.57704204692554,NA,12.4712009014367,3.20503647267553,2.13758701540187,5.70120675460775,4.14305470252736,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"ARM005","ARM005","Eurasia","Persian Belt","Armenia","Aragatsotn","Arteni","Arteni 3","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",40.32,43.98,"","Aragats","","","Obsidian","""There is a subsource of Artnei 3 known as Artnei 3b (Chataigner and Gratuze 2014).""","","""Literature suggests alternate names for this source include: Arteni C, Pokr Arteni, Talin (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31625,NA,38275,NA,562.076923076923,560.692307692308,4535,NA,37.8173076923077,NA,117.948461538462,28.3738461538462,15.6,60.4320384615385,26.8388461538462,NA,NA,342.625,20.7075,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,14.855,5.96,421.265300789196,NA,268.145390656315,NA,28.4229557242204,125.105455810951,34.5925204495753,NA,0.66324560431375,NA,2.40886877137751,7.55683530655752,1.92753511215429,8.20476888670759,1.45467918771563,NA,NA,7.1974415096415,0.453760447265512,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.0825552471924984,0.199935539601507,26
"ARM008","ARM008","Eurasia","Persian Belt","Armenia","Syunik","Bazenk","Bazenk Group General","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",39.751,45.832,"","Syunik","","","Obsidian","","","""Literature suggests alternate names for this source include: Basenk (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Nadooshan, Farhang Khademi, Akbar Adebi, Michael D. Glascock, Nasir Eskandri, and Mostafa hazaee. (2013) Provenance of Prehistoric Obsidian Artefacts from Kul Tepe, Northwestern Iran using X-Ray Fluorescence (XRF) Analysis. Journal of Archaeological Science 40 (2013) 1956-1965. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3984,NA,26,14,151,14,11,93,31,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,612.82024249386,NA,3.84276613977672,1.47685411511676,14.5980723729995,2.99136737449716,1.35915937395495,10.6254955546798,4.32440053125752,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"ARM010","ARM010","Eurasia","Persian Belt","Armenia","Kotayk","Gegham","Gegham-Alaphars","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.626,44.502,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Alaphars (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., G. Bigazzi, Y. Keheyan, S. Meloni. Characterization of Armenian Obsidians: Implications for Raw Material Supply for Prehistoric Artifacts. Journal of Radioanalytical and Nuclear Chemistry, Vol 243, No 3 (2000) 673-682. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32160,NA,31500,NA,1254,630,9656,NA,46.91,NA,138.16,226.744,NA,169.17,60.892,NA,NA,527.762,38.952,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,18.338,8.586,294.721359549996,NA,342.474487139159,NA,23.0415945787923,22.1237243569579,153.912284723994,NA,1.37099535315182,NA,2.63507311127917,17.8942109397533,NA,5.00399784049772,1.90928073202268,NA,NA,6.13496772867309,0.792409603797086,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.36313627030671,0.163683941997588,5
"ARM011","ARM011","Eurasia","Persian Belt","Armenia","Aragatsotn","Gegham","Gegham-Gyumush","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.615,44.474,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Guyumush (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., G. Bigazzi, Y. Keheyan, S. Meloni. Characterization of Armenian Obsidians: Implications for Raw Material Supply for Prehistoric Artifacts. Journal of Radioanalytical and Nuclear Chemistry, Vol 243, No 3 (2000) 673-682. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3345,NA,31450,NA,1325,720,10120,NA,54.265,NA,157.275,251.92,NA,184.01,56.96,NA,NA,645.065,39.435,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.305,9.325,173.535533905933,NA,210.355339059327,NA,30.6066017177982,29.5710678118655,88.6396103067893,NA,0.080961940777124,NA,1.29925667222985,0.269558441227157,NA,1.0265916292849,0.0649264068711945,NA,NA,2.5275514036826,0.0493198051533933,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.0563908729652599,0.023106601717798,2
"ARM012","ARM012","Eurasia","Persian Belt","Armenia","Aragatsotn","Gegham","Gegham-Nurnus","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.575,44.516,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Nurnus (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., G. Bigazzi, Y. Keheyan, S. Meloni. Characterization of Armenian Obsidians: Implications for Raw Material Supply for Prehistoric Artifacts. Journal of Radioanalytical and Nuclear Chemistry, Vol 243, No 3 (2000) 673-682. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3360,NA,32550,NA,1125,855,11370,NA,51.195,NA,138.195,268.55,NA,177.495,62.35,NA,NA,604.11,37.79,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,17.83,8.16,301.139610306789,NA,451.776695296637,NA,28.1066017177982,28.1066017177982,1128.08657865101,NA,2.21214772466386,NA,0.992700756319634,57.4125731576646,NA,8.16983458536309,0.998172798364529,NA,NA,5.10159775673127,0.821101730552665,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.133566017177982,0.144350288425444,2
"ARM020","ARM020","Eurasia","Persian Belt","Armenia","Syunik","Sevkar","Sevkar Complex","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",39.775,45.778,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Metz Sevkar, Pokr Sevkar, Greater Sevkar (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Boulanger, Matthew T, Richard S. Davis, and Michael D. Glascock. Preliminary Characterization and Regional Comparison of the Dash-i-Nawur Obsidian Source Near Ghazni, Afghanistan. Journal of Archaeological Science 39 (2012) 2320-2328. ; John F. Cherry, Elissa Z. Faro & Leah Minc. Field Survey and Geochemical Characterization of the Southern Armenian Obsidian Sources. Journal of Field Archaeology 35, 2 (2010) 147-163 ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31506.25,NA,37751.25,NA,NA,453.4375,4967.5,NA,33.91875,NA,180.5625,11.1,NA,159.375,NA,NA,NA,87.38125,36.0625,55.6,NA,NA,NA,NA,0.17,NA,NA,NA,NA,NA,34.5625,10.9625,1310.9608575874,NA,1576.30411165688,NA,NA,8.38706890143243,130.90674593052,NA,1.28346194077713,NA,7.59049602617861,7.4,NA,3.46213203435596,NA,NA,NA,12.509961392805,1.90952056147303,1.74132250993908,NA,NA,NA,NA,0.0125,NA,NA,NA,NA,NA,1.6073511889578,0.549448051533946,48
"ARM021","ARM021","Eurasia","Persian Belt","Armenia","Gegharkunik","Spitasker","Spitaksar","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.253,44.973,"","Gegham","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., G. Bigazzi, Y. Keheyan, S. Meloni. Characterization of Armenian Obsidians: Implications for Raw Material Supply for Prehistoric Artifacts. Journal of Radioanalytical and Nuclear Chemistry, Vol 243, No 3 (2000) 673-682. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32370,NA,36700,NA,420,NA,3920,NA,45.12,NA,196.1,15,NA,65.6,56.8,NA,NA,15.6,16.48,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.76,12.98,70,NA,800,NA,60,NA,90,NA,0.04,NA,0.6,0.1,NA,0.8,0.7,NA,NA,0.1,0.05,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.07,0.07,1
"ARM022","ARM022","Eurasia","Persian Belt","Armenia","Vayots Dzor","Syunik","Syunik Group General","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",39.87,45.76,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Sjunik (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Nadooshan, Farhang Khademi, Akbar Adebi, Michael D. Glascock, Nasir Eskandri, and Mostafa hazaee. (2013) Provenance of Prehistoric Obsidian Artefacts from Kul Tepe, Northwestern Iran using X-Ray Fluorescence (XRF) Analysis. Journal of Archaeological Science 40 (2013) 1956-1965. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4473.23076923077,NA,25.2307692307692,14.0769230769231,150.923076923077,23.3076923076923,12.4615384615385,96.8461538461538,28.2307692307692,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,174.178621844623,NA,1.87766904049703,0.277350098112615,6.37000181137518,1.9741924671713,1.50639661750509,4.81051199364742,2.55453342621329,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,13
"ARM023","ARM023","Eurasia","Persian Belt","Armenia","Lori","tsaghkunyats","Tsaghkunyats Group General","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.886,44.306,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Tsaghkuniats, Tsaghkunjats, Ttvakar volcano, Tzaghkuniaz Mountians, Hankavan, Tsakhkunjats, Aïkasar (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,625.684210526316,406.684210526316,6026,NA,34.0263157894737,NA,103.947368421053,118.826315789474,7.57894736842105,70.6842105263158,19.8631578947368,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,118.79393923934,15.556349186104,1518.15825920752,NA,3.53553390593274,NA,20.5060966544099,43.840620433566,1.48492424049175,24.7487373415292,2.26274169979695,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19
"ARM024","ARM024","Eurasia","Persian Belt","Armenia","Vayots Dzor","Vardensis","Vardenis","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",39.938,45.602,"","Vardenis","","","Obsidian","","","""Literature suggests alternate names for this source include: Choraphor, Khoraphor (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Nadooshan, Farhang Khademi, Akbar Adebi, Michael D. Glascock, Nasir Eskandri, and Mostafa hazaee. (2013) Provenance of Prehistoric Obsidian Artefacts from Kul Tepe, Northwestern Iran using X-Ray Fluorescence (XRF) Analysis. Journal of Archaeological Science 40 (2013) 1956-1965. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3747,NA,26,14,184,12,12,89,35,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,576.364821441891,NA,3.84276613977672,1.47685411511676,17.7883795803438,2.56402917814042,1.48271931704176,10.1684849931882,4.88238769658107,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"ARM025","ARM025","Eurasia","Persian Belt","Armenia","Aragatsotn","Arterni","Arteni 3b","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",40.32,43.98,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Pokr Arteni, Talin (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32320,NA,30450,NA,953.5,585.5,7156,NA,40.34,NA,128.425,160.26,13.9,121.975,39.825,NA,NA,569.9,40.26,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.65,9.545,284.129509039023,NA,408.124458405139,NA,248.643609138764,93.1115070607642,1657.7708630941,NA,4.44946554836957,NA,11.9356441150134,81.8723699559098,1.71748320890671,41.0665566549562,10.9788780286721,NA,NA,8.4981493398826,0.397695526217004,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.0832106781186545,0.162456890143242,4
"ARM026","ARM026","Eurasia","Persian Belt","Armenia","Syunik","Bazenk","Bazenk 1","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",39.751,45.832,"","Syunik","","","Obsidian","","","""Literature suggests alternate names for this source include: Basenk 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Nadooshan, Farhang Khademi, Akbar Adebi, Michael D. Glascock, Nasir Eskandri, and Mostafa hazaee. (2013) Provenance of Prehistoric Obsidian Artefacts from Kul Tepe, Northwestern Iran using X-Ray Fluorescence (XRF) Analysis. Journal of Archaeological Science 40 (2013) 1956-1965. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32880,NA,37640,NA,NA,541.5,4360,NA,32.37,NA,198.9,NA,NA,161.3,NA,NA,NA,49.46,18.72,30.55,NA,NA,NA,NA,0.063,NA,NA,NA,NA,NA,35.95,11.4,570,NA,1920,NA,NA,10.2,70,NA,4.29,NA,4,NA,NA,5.7,NA,NA,NA,14.54,0.2,0.59,NA,NA,NA,NA,0.003,NA,NA,NA,NA,NA,0.57,0.75,12
"ARM027","ARM027","Eurasia","Persian Belt","Armenia","Syunik","Bazenk","Bazenk 2","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",39.751,45.832,"","Syunik","","","Obsidian","","","""Literature suggests alternate names for this source include: Basenk 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Nadooshan, Farhang Khademi, Akbar Adebi, Michael D. Glascock, Nasir Eskandri, and Mostafa hazaee. (2013) Provenance of Prehistoric Obsidian Artefacts from Kul Tepe, Northwestern Iran using X-Ray Fluorescence (XRF) Analysis. Journal of Archaeological Science 40 (2013) 1956-1965. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32710,NA,36730,NA,NA,536.9,4530,NA,36.28,NA,212.1,NA,NA,165.2,NA,NA,NA,73.19,26.62,41.86,NA,NA,NA,NA,0.096,NA,NA,NA,NA,NA,38.9,12.59,350,NA,2490,NA,NA,7.4,30,NA,1.12,NA,0.8,NA,NA,7.4,NA,NA,NA,9.79,0.05,0.8,NA,NA,NA,NA,0.0131833557726357,NA,NA,NA,NA,NA,0.45,1.49354247172334,3
"ARM028","ARM028","Eurasia","Persian Belt","Armenia","Aragatsotn","Gegham","Gegham Group General","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.609,44.528,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Nurnus (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Nadooshan, Farhang Khademi, Akbar Adebi, Michael D. Glascock, Nasir Eskandri, and Mostafa hazaee. (2013) Provenance of Prehistoric Obsidian Artefacts from Kul Tepe, Northwestern Iran using X-Ray Fluorescence (XRF) Analysis. Journal of Archaeological Science 40 (2013) 1956-1965. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,381,603,3400.4,NA,29.44,14,184,9.5,17.34,49.9,44.36,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7.17173704041669,51.2406388829598,224.11551643267,NA,3.04785363242822,1.47685411511676,10.4036192797337,7.12287119900726,2.18039392015728,13.4262692466058,4.59616208181924,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10
"ARM029","ARM029","Eurasia","Persian Belt","Armenia","Kotayk","Hatis","Hatis 1","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.495,44.68,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Atis, Akunk deposit (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 1: Source Characterization. Archaeometry 56, 1 (2014) 48-69. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,365733.139722491,166435.429847413,32209.4866024035,NA,629.333333333333,465.444444444444,6224.44444444444,NA,36.4333333333333,NA,108.222222222222,82.9333333333333,10.5888888888889,63.5666666666667,21.5333333333333,NA,4.4,450,21.2,41.4,NA,NA,NA,1.8,0.47,1.4,0.2,2.6,1.8,NA,13.5,10.1,32641.4972571797,42211.8843815904,581.098985094908,NA,19.6066017177982,23.9601551083915,590.693434175952,NA,3.0167261889578,NA,4.20710678118655,6.72444263558534,1.00104076400857,4.60771644662753,1.27426406871193,NA,0.4,24,1.2,1.7,NA,NA,NA,0.172159461391866,0.0645435126368623,0.136741610116797,0.0922343492397058,0.1,0.2,NA,2.1,1.1,9
"ARM030","ARM030","Eurasia","Persian Belt","Armenia","Kotayk","Hatis","Hatis 2","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.495,44.68,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Atis, Akunk deposit (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 1: Source Characterization. Archaeometry 56, 1 (2014) 48-69. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,403567.602452404,156786.999131621,30715.2320693023,NA,1134.68421052632,481.684210526316,10834.2105263158,NA,43.0368421052632,NA,92.5789473684211,153.236842105263,10.2315789473684,92.3947368421053,19.6684210526316,NA,3.4,465,24.6,45.6,NA,NA,NA,1.9,0.45,1.4,0.21,2.8,1.6,NA,13.6,8.2,34867.0538883511,29548.3190671133,332.056562911376,NA,86.2609306503489,29.5208152801713,886.758278429838,NA,5.42591449816148,NA,4.35355339059327,15.2086832458153,0.44142135623731,6.93302127934803,0.641421356237309,NA,0.4,41,1.8,3.9,NA,NA,NA,0.1,0.07,0.136741610116797,0.01,0.3,0.1,NA,1.1,0.7,19
"ARM031","ARM031","Eurasia","Persian Belt","Armenia","Syunik","Satanakar","Satanakar 1","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",39.803,45.784,"","Syunik","","","Obsidian","","","""Literature suggests alternate names for this source include: Metz Satanakar (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; John F. Cherry, Elissa Z. Faro & Leah Minc. Field Survey and Geochemical Characterization of the Southern Armenian Obsidian Sources. Journal of Field Archaeology 35, 2 (2010) 147-163 ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32430,NA,38520,NA,NA,522.3,4650,NA,35.57,NA,203,NA,NA,163,NA,NA,NA,60.76,29.47,45.71,NA,NA,NA,NA,0.114,NA,NA,NA,NA,NA,38.05,12.35,460,NA,2530,NA,NA,27.7,60,NA,1.13,NA,3.6,NA,NA,5.9,NA,NA,NA,13.77,2.53402787928644,1.09,NA,NA,NA,NA,0.004,NA,NA,NA,NA,NA,0.59,0.64,11
"ARM032","ARM032","Eurasia","Persian Belt","Armenia","Syunik","Satanakar","Satanakar 2","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",39.803,45.784,"","Syunik","","","Obsidian","","","""Literature suggests alternate names for this source include: Metz Satanakar (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; John F. Cherry, Elissa Z. Faro & Leah Minc. Field Survey and Geochemical Characterization of the Southern Armenian Obsidian Sources. Journal of Field Archaeology 35, 2 (2010) 147-163 ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32070,NA,37500,NA,NA,577,4410,NA,37.04,NA,219,NA,NA,168.6,NA,NA,NA,69.33,23.91,38.3,NA,NA,NA,NA,0.085,NA,NA,NA,NA,NA,38.16,12.28,430,NA,1430,NA,NA,11.2,40,NA,1.72,NA,4,NA,NA,12.2,NA,NA,NA,8.06,0.51,0.48,NA,NA,NA,NA,0.005,NA,NA,NA,NA,NA,0.54,0.24,9
"ARM033","ARM033","Eurasia","Persian Belt","Armenia","Vayots Dzor","Syunik","Syunik 1","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",39.87,45.76,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Sjunik (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 1: Source Characterization. Archaeometry 56, 1 (2014) 48-69. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31306.1632784769,241.210767894802,33786.7552762325,NA,370,471,4946,NA,34.1,NA,174,3,5.9,60.8,34.9,NA,4.9,3.3,14.1,26,NA,NA,NA,0.6,0.05,1.1,0.17,3.2,2,NA,27.8,12.7,2670.66795740561,60.3026919737005,1909.32523674041,NA,18,15,2341,NA,1.6,NA,15,0.6,0.7290036642122,6.94656053467236,2.2,NA,0.8,0.363912492773908,1,1.5,NA,NA,NA,0.1,0.00686633113158109,0.1,0.01,0.31849833229197,0.1,NA,5.4,1.50659169109503,6
"ARM034","ARM034","Eurasia","Persian Belt","Armenia","Vayots Dzor","Syunik","Syunik 2","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",39.87,45.76,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Sjunik (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 1: Source Characterization. Archaeometry 56, 1 (2014) 48-69. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30861.0519522427,301.513459868503,35197.9956686059,NA,116.111111111111,130.444444444444,1129.88888888889,NA,11.1555555555556,NA,46.7777777777778,2.17777777777778,1.98888888888889,17.2222222222222,8.12222222222222,NA,5,12.7,21,38.5,NA,NA,NA,0.9,0.09,1.1,0.18,2.6,1.9,NA,26.8,12.7,1409.51919974185,24.1210767894802,2158.36765892395,NA,171.730753750619,345.068109219035,1712.04229587016,NA,31.6783837971573,NA,66.9680374315355,1.6056349186104,2.45060966544099,18.6726442764943,12.1768812973493,NA,0.3,0.2,0.8,0.2,NA,NA,NA,0.0860797306959329,0.012359396036846,0.107439836520341,0.0830109143157352,0.258779894987225,0.184309664790986,NA,0.2,2.1,9
"ARM035","ARM035","Eurasia","Persian Belt","Armenia","Vayots Dzor","Syunik","Syunik 3","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",39.87,45.76,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Sjunik (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 1: Source Characterization. Archaeometry 56, 1 (2014) 48-69. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30267.5701839303,301.513459868503,34865.9391056945,NA,543.428571428571,395.285714285714,4241.25,NA,33.9714285714286,NA,161.107142857143,12.5857142857143,7.03571428571429,68.3142857142857,30.8571428571429,NA,4.3,31.6,24.3,46.7,NA,NA,NA,NA,NA,NA,NA,NA,1.6,NA,23.8,10.9,593.481768312359,12.0605383947401,415.07070363922,NA,34.142135623731,13.8284271247462,155.374368670765,NA,5.44705627484772,NA,7.88908729652601,1.29852813742386,0.703553390593274,5.06126983722081,1.51568542494924,NA,0.5,4,2.08947667005974,2.6,NA,NA,NA,NA,NA,NA,NA,NA,0.2,NA,2.64397866971903,1.29305901046739,28
"ARM036","ARM036","Eurasia","Persian Belt","Armenia","Lori","tsaghkunyats","Tsakhkunjats 1","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.886,44.306,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Tsaghkuniats, Tsaghkunjats, Ttvakar volcano, Tzaghkuniaz Mountians, Hankavan, Tsakhkunjats, Aïkasar (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 1: Source Characterization. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31751.2746047112,723.632303684406,34865.9391056945,NA,612,437,5622,NA,32.4,NA,103,115.9,6.1,64.6,20.5,NA,2.8,895,43.9,74,NA,NA,NA,2,0.43,0.9,0.14,3.1,24.5,NA,24.5,9,5037.16388815689,60.3026919737005,747.127266550597,NA,48,31,914,NA,1.4,NA,9,18.5,1,10.7,2,NA,0.4,38,2.7,3.8,NA,NA,NA,0.1,0.04,0.1,0.02,0.3,2.6,NA,2.6,0.3,10
"ARM037","ARM037","Eurasia","Persian Belt","Armenia","Lori","tsaghkunyats","Tsakhkunjats 2","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.886,44.306,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Tsaghkuniats, Tsaghkunjats, Ttvakar volcano, Tzaghkuniaz Mountians, Hankavan, Tsakhkunjats, Aïkasar (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 1: Source Characterization. Archaeometry 56, 1 (2014) 48-69. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31306.1632784769,1085.44845552661,34201.8259798718,NA,842,377,7613,NA,33.5,NA,84,175.1,6.2,111,18.5,NA,6.8,2,18.8,36.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28.2,17,1706.26008389803,60.3026919737005,747.127266550597,NA,41,36,403,NA,3.1,NA,6,18.3,0.6,9,0.4,NA,0.578084991125216,0.220553025923581,1.61654985173346,4.82980173376143,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.13278144899482,2.01669753926106,10
"ARM039","ARM039","Eurasia","Persian Belt","Armenia","Aragatsotn","Arteni","Arteni Group General","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",40.32,43.98,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Pokr Arteni, Talin, Mez Arteni, Metz Arteni (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., G. Bigazzi, Y. Keheyan, S. Meloni. Characterization of Armenian Obsidians: Implications for Raw Material Supply for Prehistoric Artifacts. Journal of Radioanalytical and Nuclear Chemistry, Vol 243, No 3 (2000) 673-682.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32700,NA,36800,NA,420,760,3800,NA,41.97,NA,58.4,23.89,NA,67.37,39.46,NA,NA,51.57,22.65,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,18.76,8.33,400,NA,100,NA,30,70,400,NA,0.06,NA,0.03,0.06,NA,0.03,0.04,NA,NA,0.06,0.05,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.07,0.09,1
"CHI004","CHI004","Eurasia","Northeast Asia","China","Jilin","Paektusan","Paektusan Volcano 1","","23-2.6",12.8,"Stratovolcano","Inactive","Convergent","Continental","Active Continental Margin",42.042,128.041,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: PNK 1, Changbai Shan Mountains, Baekdusan 1 (Korea) (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lee, Gikil, and JongChan Kim. Obsidians from the Sinbuk Archaeological Site in Korea - Evidences for Strait Crossing and Long-Distance Exchange of Raw Material in Paleolithic Age. Journal of Archaeological Science: Reports 2 2015) 458-466. ; Jia, Peter W., Trudy Doelman, Robin Torrence, and Michael D. Glascock. New Pieces: The Acquisition and Distribution of Volcanic Glass Sources in Northeast China during the Holocene. Journal of Archaeological Science 40 (2013) 971-982. ; Chen, Yang, Youxue Zhang, David Graham, Shangguo Su, and Jinfu Deng. Geochemistry of Cenozoic Basalts and Mantle Xenoliths in Northeast China. Lithos 96 (2007) 108-126. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30600,NA,41700,NA,NA,308,10800,NA,85,NA,234.462391304348,28.4684782608696,NA,253.500217391304,79.5064285714286,NA,NA,133.256739130435,66.5215217391304,136.027826086957,NA,NA,NA,NA,0.28695652173913,NA,NA,NA,NA,NA,27.5,7.16,900,NA,2900,NA,NA,5,100,NA,18,NA,16.5773047817764,7.33048871766445,NA,75.1319241313228,21.1102125066364,NA,NA,121.490814814083,7.62021241931162,15.2614639754572,NA,NA,NA,NA,0.0624873636679329,NA,NA,NA,NA,NA,0.8,3.27,46
"CHI005","CHI005","Eurasia","Northeast Asia","China","Jilin","Paektusan","Paektusan Volcano 2","","23-2.6",12.8,"Stratovolcano","Inactive","Convergent","Continental","Active Continental Margin",42.042,128.041,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: PNK 2, Changbai Shan Mountains, Baekdusan 2 (Korea) (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lee, Gikil, and JongChan Kim. Obsidians from the Sinbuk Archaeological Site in Korea - Evidences for Strait Crossing and Long-Distance Exchange of Raw Material in Paleolithic Age. Journal of Archaeological Science: Reports 2 2015) 458-466. ; Chen, Yang, Youxue Zhang, David Graham, Shangguo Su, and Jinfu Deng. Geochemistry of Cenozoic Basalts and Mantle Xenoliths in Northeast China. Lithos 96 (2007) 108-126. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,40600,NA,36400,NA,NA,554,29700,NA,245,NA,273.013125,12.5871428571429,NA,1123.423125,128.44,NA,NA,61.97375,128.215,257.655,NA,NA,NA,NA,0.308125,NA,NA,NA,NA,NA,45.1,15.3,200,NA,2900,NA,NA,95,1600,NA,13,NA,52.5274236597449,10.5838799051412,NA,391.134434214244,39.8792519140985,NA,NA,50.7117538087243,39.3405690924449,80.6399283974459,NA,NA,NA,NA,0.0848737383956948,NA,NA,NA,NA,NA,1.1,0.2,16
"CHI013","CHI013","Eurasia","Northeast Asia","China","Jilin","Paektusan","Paektusan Volcano Group General","","23-2.6",12.8,"Stratovolcano","Inactive","Convergent","Continental","Active Continental Margin",42.042,128.041,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: PNK, Changbai Shan Mountains, Baekdusan (Korea) (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Yi, Seonbok and Yong-Joo Jwa. On the Provenance of Prehistoric Obsidian Artifacts in South Korea. Quaternary International 392 2016) 37-43. ; Jia, Peter Weiming, Trudy Doelman, Chuanjia Chen, Hailong Zhao, Sam Lin, Robin Torrence, and Michael D. Glascock. Moving Sources: A Preliminary Study of Volcanic Glass Artifact Distributions in Northeast China Using pXRF. Journal of Archaeological Science 37 2010) 1670-1677. ; Chen, Yang, Youxue Zhang, David Graham, Shangguo Su, and Jinfu Deng. Geochemistry of Cenozoic Basalts and Mantle Xenoliths in Northeast China. Lithos 96 (2007) 108-126. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3454.45841346154,NA,66324.8878605769,NA,NA,312.988942307692,6407.62740384615,NA,154.3,10.88,109.408173076923,36.3865384615385,25,125.350721153846,NA,NA,NA,201.4,72.369,149.63,42.7,NA,8.14,NA,0.336,NA,NA,NA,NA,NA,11.1475961538462,6.8,13816.7553801522,NA,8153.10108804487,NA,NA,278.07922118935,11237.8066969665,NA,1.3,0.52,25.0186940229639,20.1224569281072,7,228.457414391076,NA,NA,NA,132.2,17.0435594607792,28.4282546408502,4.75333917718201,NA,1.03669346160441,NA,0.230388613291922,NA,NA,NA,NA,NA,2.86612064714638,0.8,423
"GEO001","GEO001","Eurasia","Persian Belt","Georgia","Kvemo Kartli","Chikiana","Chikiana Group General","","2.8",2.8,"","Inactive","Convergent","Continental","Active Continental Margin",41.267,43.939,"","Kechut","","High","Obsidian","""Chikiana obsidian is abundant over its lava dome namesake, it is of 'excellent quality, very homogenous and without inclusions' (Biangi and Gratuze 2016).""","","""Literature suggests alternate names for this source include: Kojun Dag, Lake Paravani, Taparavani, Chikiani (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Le Bourdonnec, François-Xavier, Sébastian Nomade, Gérard Poupeau, Hervé Guillou, Nikolos Tushabramishvili, Marie-Hélène Moncel, David Pleurdeau, Tamar Agapishvili, Pierre Voinchet, Ana Mgeladze, and David Lordkipanidze. Multiple Origins of Bondi Cave and Ortvale Klde (NW Georgia) Obsidians and Human Mobility in Transcaucasia During the Middle and Upper Paleolithic. Journal of Archaeological Science 39 (2012) 1317-1330. ; Shackley, Steven M. Source Provenance of Obsidian Artifacts from Various Sites in the Northwestern Caucasus Mountains, Russia. Archaeological Research Facility, UC Berkeley (2012).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29806.4188099038,NA,NA,NA,775.077645880586,460.5,6570.46662478865,NA,54.1177777777778,33.8136363636364,133.25,92.3190476190476,16.152380952381,94.4,37.8794117647059,NA,4.44888888888889,858.35,31.5222222222222,64.8516129032258,NA,NA,NA,NA,0.01,NA,NA,NA,NA,20.875,16.4111111111111,5.77578947368421,730.823475581655,NA,NA,NA,146.226882665378,32.0133900556805,872.759442008016,NA,15.3390298174932,12.4190386347028,8.10094418684277,11.9611434603712,1.61750891142337,15.4297524121937,23.439170560874,NA,0.397397885440479,104.499242460436,2.82113405661367,15.0225115257473,NA,NA,0.583333333333333,NA,0.00137326622631622,NA,NA,NA,NA,1.35620268186054,2.10733176901618,0.863346543302089,45
"GEO002","GEO002","Eurasia","Persian Belt","Georgia","Kvemo Kartli","Chikiana","Chikiana 1a","","2.8",2.8,"","Inactive","Convergent","Continental","Active Continental Margin",41.267,43.939,"","Kechut","","High","Obsidian","""Chikiana obsidian is abundant over its lava dome namesake, it is of 'excellent quality, very homogenous and without inclusions' (Biangi and Gratuze 2016).""","","""Literature suggests alternate names for this source include: Kojun Dag, Lake Paravani, Taparavani, Chikiani (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; .""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28328.8630741099,513.778935615929,38014.942177304,NA,554.266666666667,461.133333333333,4869.13333333333,NA,48.2,NA,129.866666666667,56.7333333333333,10.1066666666667,59.0666666666667,19.8,NA,4.56666666666667,489.266666666667,17.4733333333333,36.6666666666667,10.7333333333333,NA,NA,2.12666666666667,0.542,NA,NA,NA,NA,NA,12.2333333333333,5.68866666666667,846.70874481827,13.9014195228419,694.168044642315,NA,38.1397180802126,8.67563638395862,460.947295820042,NA,4.61673972780421,NA,6.43502321748133,3.32665998663324,0.254857569933445,1.75119007154183,0.560611910581388,NA,0.241029537806548,19.4659654146361,0.867234246380549,1.4489733639801,0.322194853791186,NA,NA,0.0625261849909605,0.122544452575965,NA,NA,NA,NA,NA,0.55118919057754,0.141616517734472,15
"GEO003","GEO003","Eurasia","Persian Belt","Georgia","Kvemo Kartli","Chikiana","Chikiana 1b","","2.8",2.8,"","Inactive","Convergent","Continental","Active Continental Margin",41.267,43.939,"","Kechut","","High","Obsidian","""Chikiana obsidian is abundant over its lava dome namesake, it is of 'excellent quality, very homogenous and without inclusions' (Biangi and Gratuze 2016).""","","""Literature suggests alternate names for this source include: Kojun Dag, Lake Paravani, Taparavani, Chikiani (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; .""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27868.9147036679,547.414437139037,37872.8957587253,NA,598,459.444444444444,5409.66666666667,NA,46.6666666666667,NA,125.333333333333,59.4444444444444,10.3222222222222,66.1111111111111,19.7777777777778,NA,4.37777777777778,520.888888888889,18.9888888888889,38.5444444444444,11.4222222222222,NA,NA,2.20333333333333,0.568888888888889,NA,NA,NA,NA,NA,12.6555555555556,5.48111111111111,627.29296343394,32.7218901367245,873.40362359816,NA,26.9536639438871,9.8375697089158,207.032606127634,NA,2.95803989154981,NA,5.1234753829798,2.35112266327765,0.494413232473044,2.71313676601662,0.440958551844098,NA,0.204803428790742,19.4450793547137,1.09023442942842,2.2776693741142,0.359783885748715,NA,NA,0.0680073525436772,0.0301846171271247,NA,NA,NA,NA,NA,0.589726867098471,0.137608543016453,9
"GEO004","GEO004","Eurasia","Persian Belt","Georgia","Kvemo Kartli","Chikiana","Chikiana 2","","2.8",2.8,"","Inactive","Convergent","Continental","Active Continental Margin",41.267,43.939,"","Kechut","","High","Obsidian","""Chikiana obsidian is abundant over its lava dome namesake, it is of 'excellent quality, very homogenous and without inclusions' (Biangi and Gratuze 2016).""","","""Literature suggests alternate names for this source include: Kojun Dag, Lake Paravani, Taparavani, Chikiani (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; .""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27485.6243949662,693.480957697556,37688.4198904412,NA,706,418,6248,NA,45,NA,116.5,73,9.7,82.5,18,NA,3.9,673.5,24.65,48.85,13.3,NA,NA,2.335,0.73,NA,NA,NA,NA,NA,13.35,5.11,1101.59433007113,42.6404424184069,352.199171058155,NA,9.89949493661167,18.3847763108502,176.776695296637,NA,5.65685424949238,NA,0.707106781186548,2.82842712474619,0.707106781186548,3.53553390593274,2.51094224395598,NA,0.33154874491005,0.707106781186548,2.05060966544099,2.05060966544099,0.565685424949237,NA,NA,0.0919238815542511,0.197989898732233,NA,NA,NA,NA,NA,0.777817459305202,0.113137084989848,2
"GEO005","GEO005","Eurasia","Persian Belt","Georgia","Kvemo Kartli","Chikiana","Chikiana 3a","","2.8",2.8,"","Inactive","Convergent","Continental","Active Continental Margin",41.267,43.939,"","Kechut","","High","Obsidian","""Chikiana obsidian is abundant over its lava dome namesake, it is of 'excellent quality, very homogenous and without inclusions' (Biangi and Gratuze 2016).""","","""Literature suggests alternate names for this source include: Kojun Dag, Lake Paravani, Taparavani, Chikiani (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; .""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27485.6243949661,830.837089415429,37042.7543514469,NA,824.888888888889,387,6964.61111111111,NA,44.5555555555556,NA,113.666666666667,97.2777777777778,9.95,100.722222222222,17.1666666666667,NA,3.7,843.111111111111,29.5111111111111,55.3055555555556,15.2944444444444,NA,NA,2.54277777777778,0.850555555555556,NA,NA,NA,NA,NA,14.0333333333333,4.80777777777778,1622.17662610972,81.5774264158537,1507.10056825814,NA,29.2290928576486,17.746582106721,900.967332363903,NA,4.04710822283273,NA,4.92293551833122,10.709015199165,0.609966247860824,5.07364071110278,0.785905247993376,NA,0.181497042594606,52.9937719857819,2.01286710612701,2.85048442162179,0.566176258382101,NA,NA,0.0923424289425318,0.131751647929072,NA,NA,NA,NA,NA,1.06494959836549,0.150979373564173,18
"GEO006","GEO006","Eurasia","Persian Belt","Georgia","Kvemo Kartli","Chikiana","Chikiana 3b","","2.8",2.8,"","Inactive","Convergent","Continental","Active Continental Margin",41.267,43.939,"","Kechut","","High","Obsidian","""Chikiana obsidian is abundant over its lava dome namesake, it is of 'excellent quality, very homogenous and without inclusions' (Biangi and Gratuze 2016).""","","""Literature suggests alternate names for this source include: Kojun Dag, Lake Paravani, Taparavani, Chikiani (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; .""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28125.1010003227,1126.45428606873,36987.7805426982,NA,1012.88,374.84,8225.4,NA,52.24,NA,109.24,123.28,9.74,120.04,15.72,NA,3.416,1008.2,32.46,59.28,16.688,NA,NA,2.672,0.9348,NA,NA,NA,NA,NA,13.488,4.286,1178.88384978832,123.975451709342,1335.35842516888,NA,67.6469511508094,14.0317497127051,636.894483673185,NA,27.3286784654265,NA,4.76340214552582,7.75951029382654,0.586657196893268,8.19796722771363,0.613731754650732,NA,0.179536440126603,39.9802034345333,1.86346451535842,2.55571255556384,0.667907179179862,NA,NA,0.114600756251141,0.104208125083092,NA,NA,NA,NA,NA,0.791264810287934,0.153133928311136,25
"GRE006","GRE006","Eurasia","Mediterranean","Greece","South Aegean","Melos","Melos-Adamas","","65.5-0",32.75,"Stratovolcano","Inactive","Convergent","Continental","Active Continental Margin",36.729,24.519,"","","South Aegean Volcanic Arc","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Milic, Marina. PXRF Characterization of Obsidian from Central Anatolia, the Aegean and Central Europe. Journal of Archaeological Science 41 (2014) 285-296. ; Robertson, A. H. F. and J. E. Dixon. Introduction: Aspects of the Geological Evolution of the Eastern Mediterranean. Geological Society of London, Special Publication 17 (1984) 1-74. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,882.875,489.5,5633.25,NA,25.25,NA,108.375,88.375,NA,94.5,NA,NA,NA,345.875,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,15.625,NA,NA,NA,NA,NA,NA,47.5948301514236,179.516811787325,237.859352199091,NA,2.25198325291921,NA,3.20434972230828,29.0021550923375,NA,33.8441807616697,NA,NA,NA,44.9171857024521,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.68501801601221,NA,NA,8
"GRE007","GRE007","Eurasia","Mediterranean","Greece","South Aegean","Melos","Melos-Dhemengaki","","65.5-0",32.75,"Stratovolcano","Inactive","Convergent","Continental","Active Continental Margin",36.71,24.535,"","","South Aegean Volcanic Arc","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Milic, Marina. PXRF Characterization of Obsidian from Central Anatolia, the Aegean and Central Europe. Journal of Archaeological Science 41 (2014) 285-296. ; Robertson, A. H. F. and J. E. Dixon. Introduction: Aspects of the Geological Evolution of the Eastern Mediterranean. Geological Society of London, Special Publication 17 (1984) 1-74. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1162.36363636364,386.181818181818,7053,NA,26.7272727272727,NA,97,109.545454545455,NA,114.363636363636,NA,NA,NA,324.818181818182,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,15.4545454545455,NA,NA,NA,NA,NA,NA,50.2280254982669,21.5769237001857,171.129775316863,NA,4.64953565618996,NA,2.96647939483827,3.44568241031109,NA,4.65344447205997,NA,NA,NA,34.1520663556927,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.54415551268535,NA,NA,11
"GRE010","GRE010","Eurasia","Mediterranean","Greece","South Aegean","Melos","Melos Group General","","65.5-0",32.75,"Stratovolcano","Inactive","Convergent","Continental","Active Continental Margin",36.729,24.519,"","","South Aegean Volcanic Arc","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gratuze, B. Obsidian Characterization by Laser Ablation ICP-MS and its Application to Prehistoric Trade in the Mediterranean and the Near East: Sources and Distribution of Obsidian within Aegean and Anatolia. Journal of Archaeological Science (1999) 26, 891-881. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Robertson, A. H. F. and J. E. Dixon. Introduction: Aspects of the Geological Evolution of the Eastern Mediterranean. Geological Society of London, Special Publication 17 (1984) 1-74. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23,NA,116.777777777778,105.111111111111,15.1111111111111,110.222222222222,7.88888888888889,NA,NA,474.333333333333,27.5555555555556,46.4444444444444,NA,NA,NA,NA,0.38,NA,NA,13,4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.39937004672556,NA,2.20710678118655,1.85355339059327,1.35355339059327,8.47487373415292,0.853553390593274,NA,NA,4.56066017177982,2.91421356237309,3.53553390593274,NA,NA,NA,NA,0.0521841166000163,NA,NA,1.29389947493613,0.388020346928391,NA,NA,NA,9
"HUN001","HUN001","Eurasia","Carpathian Mountains","Hungary","Borsod-Abauj-Zemplen","Carpathian","Caparthian 1","","13-19",16,"","Inactive","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",48.442,21.585,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Carpathian Mountains 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Milic, Marina. PXRF Characterization of Obsidian from Central Anatolia, the Aegean and Central Europe. Journal of Archaeological Science 41 (2014) 285-296. ; Thrope, Olwen Williams, S.E. Warren, and J.G. Nandris. The Distribution and Provenance of Archaeological Obsidian in Central and Eastern Europe. Journal of Archaeological Science 11 (1984) 183-212. ; Odddone, M., P. Matron, G. Bigazzi, K. T. Biro. Chemical Characteristics of Carpathian Obsidian Sources by Instrumentation and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry, Vol 240, No 1 (1999) 147-153. ; Pecskay, Zoltan, Jaroslav Lexa, Alexandru Szakas, Ioan Seghedi, Kadosa Baloghi, Vlastimil Konecny, Tibor Zelenka, Marinel Kovacs, Terez Poka, Alexandrina Fulop, Emo Matron, Cristian Panaiotu, and Vladica Cvetkovic. Geochronology of Neogene Magmatism in the Carpathian Arc and Intra-Carpathian Area. Geologica Carpathica 56, 6 (2006) 511-530.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24765.8914728682,NA,36801.25,NA,383.426086956522,376.165217391304,8045.64150943396,0.28,71.8959130434783,NA,202.433962264151,77.7826086956522,NA,76.9478260869565,1.955,46.52125,56.9256589147287,563.637735849057,28.0441860465116,59.4503875968992,NA,0.7,NA,NA,0.38,NA,NA,NA,NA,33.1428571428571,17.3530232558139,9.39736434108527,2844.64740095643,NA,386.589489256759,1.7,63.5251168609341,28.5846212569154,976.86267733983,0.11,17.2553716628413,NA,29.6769982551857,2.75524686113163,NA,3.64894573266413,0.0605838744494796,0.284420465748692,21.751954421854,207.443750602262,3.95650530006791,8.88297266942794,NA,0.18,NA,NA,0.0521841166000163,NA,NA,NA,NA,3.89138242053607,2.4594502576046,2.52665943219585,265
"HUN002","HUN002","Eurasia","Carpathian Mountains","Hungary","Borsod-Abauj-Zemplen","Carpathian","Caparthian 2 Group General","","13-19",16,"","Inactive","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",48.345,21.487,"","","","","Obsidian","""The Carpathian 2 source has two additional subsources, 2A and 2B (Thrope et al 1984).""","","""Literature suggests alternate names for this source include: Carpathian Mountains 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Milic, Marina. PXRF Characterization of Obsidian from Central Anatolia, the Aegean and Central Europe. Journal of Archaeological Science 41 (2014) 285-296. ; Odddone, M., P. Matron, G. Bigazzi, K. T. Biro. Chemical Characteristics of Carpathian Obsidian Sources by Instrumentation and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry, Vol 240, No 1 (1999) 147-153. ; Pecskay, Zoltan, Jaroslav Lexa, Alexandru Szakas, Ioan Seghedi, Kadosa Baloghi, Vlastimil Konecny, Tibor Zelenka, Marinel Kovacs, Terez Poka, Alexandrina Fulop, Emo Matron, Cristian Panaiotu, and Vladica Cvetkovic. Geochronology of Neogene Magmatism in the Carpathian Arc and Intra-Carpathian Area. Geologica Carpathica 56, 6 (2006) 511-530.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30277.7777777778,NA,39322.2222222222,NA,825.507692307692,344.646153846154,9938.65384615385,NA,80.8092307692308,NA,180.230769230769,224.146153846154,NA,150.446153846154,2.32666666666667,45.9377777777778,12.2866666666667,203.046153846154,46,66.2111111111111,NA,NA,NA,NA,NA,NA,NA,NA,NA,33.5,22.5011111111111,5.37888888888889,499.669893706017,NA,825.567585173648,NA,256.296196628723,25.7493686155545,1243.25086557887,NA,14.4924204134486,NA,19.0613657573995,191.275735677418,NA,11.6820049945565,0.460279010778227,0.442402191176977,1.63936311962478,81.8789630107652,5.34257905053798,5.64735773599319,NA,NA,NA,NA,NA,NA,NA,NA,NA,5.8309518948453,2.92773837565421,0.863830273203002,26
"HUN011","HUN011","Eurasia","Carpathian Mountains","Hungary","Borsod-Abauj-Zemplen","Carpathian","Caparthian 2A","","13-19",16,"","Inactive","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",48.345,21.487,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Carpathian Mountains 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Milic, Marina. PXRF Characterization of Obsidian from Central Anatolia, the Aegean and Central Europe. Journal of Archaeological Science 41 (2014) 285-296. ; Odddone, M., P. Matron, G. Bigazzi, K. T. Biro. Chemical Characteristics of Carpathian Obsidian Sources by Instrumentation and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry, Vol 240, No 1 (1999) 147-153. ; Pecskay, Zoltan, Jaroslav Lexa, Alexandru Szakas, Ioan Seghedi, Kadosa Baloghi, Vlastimil Konecny, Tibor Zelenka, Marinel Kovacs, Terez Poka, Alexandrina Fulop, Emo Matron, Cristian Panaiotu, and Vladica Cvetkovic. Geochronology of Neogene Magmatism in the Carpathian Arc and Intra-Carpathian Area. Geologica Carpathica 56, 6 (2006) 511-530.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27100,NA,NA,NA,NA,NA,11800,0.53,NA,NA,219,NA,NA,NA,NA,NA,79.7,621,39.8,79.7,NA,0.73,NA,NA,0.57,NA,NA,NA,NA,NA,24.5,5.21,1300,NA,NA,1.4,NA,NA,700,0.06,NA,NA,48,NA,NA,NA,NA,NA,13.4,189,2.08,13.4,NA,0.16,NA,NA,0.07,NA,NA,NA,NA,NA,2.7,1.59,16
"HUN012","HUN012","Eurasia","Carpathian Mountains","Hungary","Borsod-Abauj-Zemplen","Carpathian","Caparthian 2B","","13-19",16,"","Inactive","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",48.345,21.487,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Carpathian Mountains 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Milic, Marina. PXRF Characterization of Obsidian from Central Anatolia, the Aegean and Central Europe. Journal of Archaeological Science 41 (2014) 285-296. ; Odddone, M., P. Matron, G. Bigazzi, K. T. Biro. Chemical Characteristics of Carpathian Obsidian Sources by Instrumentation and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry, Vol 240, No 1 (1999) 147-153. ; Pecskay, Zoltan, Jaroslav Lexa, Alexandru Szakas, Ioan Seghedi, Kadosa Baloghi, Vlastimil Konecny, Tibor Zelenka, Marinel Kovacs, Terez Poka, Alexandrina Fulop, Emo Matron, Cristian Panaiotu, and Vladica Cvetkovic. Geochronology of Neogene Magmatism in the Carpathian Arc and Intra-Carpathian Area. Geologica Carpathica 56, 6 (2006) 511-530.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,26600,NA,NA,NA,NA,NA,14300,1.45,NA,NA,209,NA,NA,NA,NA,NA,85.9,672,44.3,85.9,NA,0.72,NA,NA,0.63,NA,NA,NA,NA,NA,25.7,6.21,1600,NA,NA,1,NA,NA,1000,0.14,NA,NA,21,NA,NA,NA,NA,NA,7.3025736378906,223,3.80921055488257,11.4925199149614,NA,0.0971314412154519,NA,NA,0.07,NA,NA,NA,NA,NA,2.1,1.26,6
"HUN013","HUN013","Eurasia","Carpathian Mountains","Hungary","Borsod-Abauj-Zemplen","Tolcsva","Tolcsva Group General","","13-19",16,"","Inactive","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",48.299,21.436,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Cann, J. R. and Colin Renfrew. Characterization of Obsidian and its Application to the Mediterranean Region. The Prehistory Society 8 (111-122) 1964. ; Glascock, Michael D., Alex W. Barker, Sandra Băcueţ Crişan, Florin Draşovean, Mihai Gligor, and Dimitrie Negrei. Sourcing Obsidian Artifacts from Archaeological Sites in Central and Western Romania by X-Ray Fluorescence. Analele Banatului, S. N. Arheologie No. 24, 2016. ; Thrope, Olwen Williams, S.E. Warren, and J.G. Nandris. The Distribution and Provenance of Archaeological Obsidian in Central and Eastern Europe. Journal of Archaeological Science 11 (1984) 183-212. ; Pecskay, Zoltan, Jaroslav Lexa, Alexandru Szakas, Ioan Seghedi, Kadosa Baloghi, Vlastimil Konecny, Tibor Zelenka, Marinel Kovacs, Terez Poka, Alexandrina Fulop, Emo Matron, Cristian Panaiotu, and Vladica Cvetkovic. Geochronology of Neogene Magmatism in the Carpathian Arc and Intra-Carpathian Area. Geologica Carpathica 56, 6 (2006) 511-530.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,26921.4285714286,205,NA,NA,NA,331.866666666667,11531.7885245902,0.550892857142857,10.0666666666667,12,209.518032786885,43.2,16.22,63.56,11.075,NA,40.1696428571429,562.879310344828,41.3275862068966,85.575,NA,0.755714285714286,NA,NA,0.54125,NA,NA,4.5775,0.980833333333333,44,24.2796610169492,5.16446428571429,1318.30923928453,49.4974746830583,NA,0.45,NA,20.2124549061546,1376.57262984593,0.0623396678728199,1.9731531449265,1.26587495581437,47.0078314122685,31.9602096363588,10.0753163722039,40.9531805846628,12.6368179011437,NA,23.6884711000929,87.8003286845788,8.12335205128611,4.00866302262565,NA,0.118241679807703,NA,NA,0.0331433982504195,NA,NA,0.444667904682298,0.108078955426395,7.00810755296767,3.17142435665762,0.533067545360352,61
"HUN014","HUN014","Eurasia","Carpathian Mountains","Hungary","Borsod-Abauj-Zemplen","Tokaj","Tokaj Upper Section","","13-19",16,"","Inactive","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",48.113,21.394,"","","","","Obsidian","""The Tokaj source is found in the southern Zemplen Mountains, and nodules average 8mm across - making this an unfit source for tool manufacturing (Williams and Nandris 1977).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Thrope, Olwen Williams, S.E. Warren, and J.G. Nandris. The Distribution and Provenance of Archaeological Obsidian in Central and Eastern Europe. Journal of Archaeological Science 11 (1984) 183-212. ; Pecskay, Zoltan, Jaroslav Lexa, Alexandru Szakas, Ioan Seghedi, Kadosa Baloghi, Vlastimil Konecny, Tibor Zelenka, Marinel Kovacs, Terez Poka, Alexandrina Fulop, Emo Matron, Cristian Panaiotu, and Vladica Cvetkovic. Geochronology of Neogene Magmatism in the Carpathian Arc and Intra-Carpathian Area. Geologica Carpathica 56, 6 (2006) 511-530. ; Williams, Olwen, and John Nandris. The Hungarian and Slovak Sources of Archaeological Obsidian: an Interim Report on Further Fieldwork, with a Note on Tektites. Journal of Archaeological Science 4 (1997) 207-219.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25310,NA,NA,NA,NA,NA,10290,0.301,NA,NA,342.9,NA,NA,NA,NA,NA,13.32,183,43.89,108.32,NA,0.719,NA,NA,0.18,NA,NA,4.69,0.952,NA,28.59,5.722,1483.83751861183,NA,NA,0.26,NA,NA,861.000593588748,0.0434100128035961,NA,NA,26.143383687193,NA,NA,NA,NA,NA,0.77466401061363,42.2971504416867,2.19809960296525,5.78952089481376,NA,0.14922338247977,NA,NA,0.0453540097839643,NA,NA,0.426848919408261,0.0697853852894716,NA,1.94280568850206,0.483785604320386,10
"HUN015","HUN015","Eurasia","Carpathian Mountains","Hungary","Borsod-Abauj-Zemplen","Tokaj","Tokaj Lower Section","","13-19",16,"","Inactive","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",48.113,21.394,"","","","","Obsidian","""The Tokaj source is found in the southern Zemplen Mountains, and nodules average 8mm across - making this an unfit source for tool manufacturing (Williams and Nandris 1977).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Thrope, Olwen Williams, S.E. Warren, and J.G. Nandris. The Distribution and Provenance of Archaeological Obsidian in Central and Eastern Europe. Journal of Archaeological Science 11 (1984) 183-212. ; Pecskay, Zoltan, Jaroslav Lexa, Alexandru Szakas, Ioan Seghedi, Kadosa Baloghi, Vlastimil Konecny, Tibor Zelenka, Marinel Kovacs, Terez Poka, Alexandrina Fulop, Emo Matron, Cristian Panaiotu, and Vladica Cvetkovic. Geochronology of Neogene Magmatism in the Carpathian Arc and Intra-Carpathian Area. Geologica Carpathica 56, 6 (2006) 511-530. ; Williams, Olwen, and John Nandris. The Hungarian and Slovak Sources of Archaeological Obsidian: an Interim Report on Further Fieldwork, with a Note on Tektites. Journal of Archaeological Science 4 (1997) 207-219.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20883.3333333333,NA,NA,NA,NA,NA,8800,0.418333333333333,NA,NA,169.833333333333,NA,NA,NA,NA,NA,11.5833333333333,155,37.4833333333333,88.3,NA,0.55,NA,NA,0.218333333333333,NA,NA,3.80333333333333,0.753333333333333,NA,25.6166666666667,3.93,1182.72231493203,NA,NA,0.27,NA,NA,603.553390593274,0.102192515134006,NA,NA,10.0990344391495,NA,NA,NA,NA,NA,1.61934358391885,29.0364031172107,1.61371743485713,3.65540692173246,NA,0.0512132034355964,NA,NA,0.0770968586209513,NA,NA,0.221885856541902,0.045092497528229,NA,1.9642609123207,0.237275382291719,6
"IRN001","IRN001","Eurasia","Persian Belt","Iran","East Azerbaijan","Lake Urmia","Lake Urmia A","","0.8-1.2",1,"","Active","Transform","Continental","Active Continental Margin",37.532,45.929,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Niknami, K. A., A. C. Amirkhiz, and M. D. Shackley. Provenance Studies of Chalcolithic Obsidian Artefacts from Near Lake Urmia, Northwestern Iran Using WDXRF Analysis. Archaeometry 52, 1 (2010) 19-30.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29674.0884156179,NA,NA,NA,593.405107661492,518.882122416758,6854.29269209092,NA,64.4,34.8,144.7,57.4,23.6,102.3,NA,NA,NA,32.2,NA,62,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1854.63052597612,NA,NA,NA,107.891837756635,92.9341114776283,1054.32964600679,NA,63.5,10.9,14.6,12.2646062354383,8.5,11.6880451101477,NA,NA,NA,14.3,NA,10.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,47
"IRN002","IRN002","Eurasia","Persian Belt","Iran","East Azerbaijan","Lake Urmia","Lake Urmia B","","0.8-1.2",1,"","Active","Transform","Continental","Active Continental Margin",37.532,45.929,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Niknami, K. A., A. C. Amirkhiz, and M. D. Shackley. Provenance Studies of Chalcolithic Obsidian Artefacts from Near Lake Urmia, Northwestern Iran Using WDXRF Analysis. Archaeometry 52, 1 (2010) 19-30.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29599.9031945789,NA,NA,NA,755.242864296445,681.516817502608,9582.02141649446,NA,113.8,43.2,157.2,56.8,35.8,155.8,NA,NA,NA,35.6,NA,90,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2003.00096805421,NA,NA,NA,215.78367551327,139.401167216443,1473.90981125439,NA,64.1,8.3,30.1,3.3,10.9,31.2,NA,NA,NA,6.8,NA,18.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4
"IRN003","IRN003","Eurasia","Persian Belt","Iran","East Azerbaijan","Lake Urmia","Lake Urmia C","","0.8-1.2",1,"","Active","Transform","Continental","Active Continental Margin",37.532,45.929,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Niknami, K. A., A. C. Amirkhiz, and M. D. Shackley. Provenance Studies of Chalcolithic Obsidian Artefacts from Near Lake Urmia, Northwestern Iran Using WDXRF Analysis. Archaeometry 52, 1 (2010) 19-30.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,35460.5356566634,NA,NA,NA,551.447170756134,549.860159575968,12729.4007138831,NA,99.4,39.8,154.2,58.4,52.8,174,NA,NA,NA,64.6,NA,74.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,964.407873507583,NA,NA,NA,17.9819729594392,7.74450928980236,1958.04077115546,NA,32.4,8.8,18.1,2.1,6.8,6,NA,NA,NA,12.9,NA,2.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"ITL001","ITL001","Eurasia","Mediterranean","Italy","Sicily","Lipari","Lipari Group General","","8-0",4,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",38.494,14.937,"","","","High","Obsidian","""Lipari glass is high quality, transparent, and black (Barca et al 2007).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Barca, Donatella, Anna Maria de Francesco, Gino Mirocle Crisci. Application of Laser Ablation ICP-MS for Characterisation of Obsidian Fragments from Peri-Tyrrhenian Area. Journal of Cultural Heritage 8 (2007) 141-150. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Peccerillo, Angelo. Plio-Quaternary Magmatism in Italy. Episodes 26, 3 (2003) 222-226. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,284,15.75,39.8333333333333,150.833333333333,33.1666666666667,NA,15.5,19.3333333333333,59.3333333333333,112.416666666667,NA,NA,NA,NA,0.14,NA,NA,NA,NA,28.625,47.875,14,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,11.3390050389064,2.32523582806986,3.84164781287484,15.7812561637045,4.50831949054874,NA,0.962140470884727,5.28373712969951,8.51455684561405,13.6415419460802,NA,NA,NA,NA,0.0354562104171167,NA,NA,NA,NA,3.02076149339864,3.09088521763126,1.0690449676497,12
"ITL002","ITL002","Eurasia","Mediterranean","Italy","Sardinia","Monte Arci","Monte Arci - Conca Cannas","","5.3-2.6",3.95,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Barca, Donatella, Anna Maria de Francesco, Gino Mirocle Crisci. Application of Laser Ablation ICP-MS for Characterisation of Obsidian Fragments from Peri-Tyrrhenian Area. Journal of Cultural Heritage 8 (2007) 141-150. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,262.24,28.28,35.52,88.08,53.28,NA,4.6,126.72,25,56.72,NA,NA,NA,NA,0.3,NA,NA,NA,NA,35.8,18,6.18,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12.9363697612349,3.15252661360776,2.42087052914651,7.33580318091482,3.14647806600511,NA,0.824621125123532,13.6527206023271,3.91986911947076,8.74510852287855,NA,NA,NA,NA,0.090921211313239,NA,NA,NA,NA,6.89283041363351,3.46410161513775,1.0932113753118,25
"ITL003","ITL003","Eurasia","Mediterranean","Italy","Sardinia","Monte Arci","Monte Arci - Crucuc Island Abis","","5.3-2.6",3.95,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Barca, Donatella, Anna Maria de Francesco, Gino Mirocle Crisci. Application of Laser Ablation ICP-MS for Characterisation of Obsidian Fragments from Peri-Tyrrhenian Area. Journal of Cultural Heritage 8 (2007) 141-150. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,248.5,75.75,23.25,146.75,32.75,NA,3.875,471.5,39.75,85.5,NA,NA,NA,NA,0.7025,NA,NA,NA,NA,35,23,5.175,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12.1243556529821,3.09569593683445,2.21735578260835,10.2753750945322,0.957427107756338,NA,0.25,22.4722050542442,3.5,5.06622805119022,NA,NA,NA,NA,0.118145390656315,NA,NA,NA,NA,2.94392028877595,1.82574185835055,0.43493294502333,4
"ITL004","ITL004","Eurasia","Mediterranean","Italy","Sardinia","Monte Arci","Monte Arci - Perdas Urias","","5.3-2.6",3.95,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Barca, Donatella, Anna Maria de Francesco, Gino Mirocle Crisci. Application of Laser Ablation ICP-MS for Characterisation of Obsidian Fragments from Peri-Tyrrhenian Area. Journal of Cultural Heritage 8 (2007) 141-150. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,180.421052631579,125.842105263158,24.1578947368421,223.210526315789,29.3157894736842,NA,2.225,938.105263157895,66.9473684210526,131.052631578947,NA,NA,NA,NA,1.13375,NA,NA,NA,NA,35.625,26.75,3.6625,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7.51109795285896,11.5166886606372,1.26423276829637,10.6140995356002,1.74827467136541,NA,0.183225076262581,77.0747191811686,5.35249521072455,12.2185557022209,NA,NA,NA,NA,0.232067570209319,NA,NA,NA,NA,3.70086862390825,2.91547594742265,0.570557371598785,19
"ITL006","ITL006","Eurasia","Mediterranean","Italy","Sicily","Pantelleria","Pantelleria Group General","","0.3-0.005",0.1525,"Shield","Active","Convergent","Continental","Active Continental Margin",36.784,12.009,"","","","","Obsidian","""Pantelleria obsidian is green, contains microlites, and is common on its island namesake. Subsources are distinguished by their peralkaline character and Zr content (Barca et al 2007).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Barca, Donatella, Anna Maria de Francesco, Gino Mirocle Crisci. Application of Laser Ablation ICP-MS for Characterisation of Obsidian Fragments from Peri-Tyrrhenian Area. Journal of Cultural Heritage 8 (2007) 141-150. ; Peccerillo, Angelo. Plio-Quaternary Magmatism in Italy. Episodes 26, 3 (2003) 222-226. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,180.2,3.552,171.1,1786,383.2,NA,2.39,28.6,232.4,434.7,NA,NA,NA,NA,4.42,NA,NA,NA,NA,16.1,34.8,10.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33.8059823765624,1.05945268889177,39.4840333411987,342.451618642855,75.2311992017496,NA,0.71094616142465,9.6171143743271,48.0328591232664,83.2613689267451,NA,NA,NA,NA,0.370135110466435,NA,NA,NA,NA,3.5418137224372,7.16162613439775,2.06559111797729,10
"ITL008","ITL008","Eurasia","Mediterranean","Italy","Sardinia","Sardinia","Sardinia-A","","5.3-2.6",12.8,"","Active","Intraplate","Continental","Active Continental Margin",39.72,8.74,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: SA Type (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Freund, Kyle P. Obsidian Consumption in Chalcolithic Sardinia: A View from Bingia 'e Monti. Journal of Archaeological Science 41 (2014) 242-250. ; Terradas, Xavier, Bernard Gratuze, Josep Bosch, Roser Enrich, Xavier Esteve, F. Xavier Oms, Genís Ribé. Neolithic Diffusion of Obsidian in the Western Mediterranean: New Data from Iberia. Journal of Archaeological Science 41 (2014) 69-78. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25233,NA,40870,NA,35.6644736842105,84.7171052631579,2751.63402889246,NA,87.8636363636364,23,84.7752808988764,9.16837881219904,10.2290584415584,60.1219903691814,12.9951298701299,NA,NA,155.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,482,NA,971,NA,51.7007024440194,30.6043118659212,1300.82792151654,NA,9.18722657276032,1,29.5059598164287,4.60432899672725,6.01262909717782,7.77262944521557,8.7420668408201,NA,NA,17.1164081679372,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,623
"ITL009","ITL009","Eurasia","Mediterranean","Italy","Sardinia","Sardinia","Sardinia-B1","","5.3-2.6",12.8,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","""There are two subsources, Sardinia B1 and Sardinia B2 (Terradas et al 2014).""","","""Literature suggests alternate names for this source include: SB Type (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Terradas, Xavier, Bernard Gratuze, Josep Bosch, Roser Enrich, Xavier Esteve, F. Xavier Oms, Genís Ribé. Neolithic Diffusion of Obsidian in the Western Mediterranean: New Data from Iberia. Journal of Archaeological Science 41 (2014) 69-78. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25468,NA,41771,NA,832,350,11713.0909090909,NA,69.5454545454545,24,242.272727272727,68.7272727272727,28.2,139,37.2,NA,NA,515,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,393,NA,678,NA,53,13,1453.50749243214,NA,5.67840784883063,1,12.7387014414564,6.26907484122731,4.14728827066554,18.2596281081814,6.53452370108182,NA,NA,127.730184373154,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,11
"ITL010","ITL010","Eurasia","Mediterranean","Italy","Sardinia","Sardinia","Sardinia-C","","5.3-2.6",12.8,"","Active","Intraplate","Continental","Active Continental Margin",39.792,8.665,""," ","","","Obsidian","""There are two subsources, Sardinia C1 and Sardinia C2 (sometimes called Sardinia D) (Terradas et al 2014).""","","""Literature suggests alternate names for this source include: SC Type (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Freund, Kyle P. Obsidian Consumption in Chalcolithic Sardinia: A View from Bingia 'e Monti. Journal of Archaeological Science 41 (2014) 242-250. ; Freund, Kyle P. Obsidian Consumption in Chalcolithic Sardinia: A View from Bingia 'e Monti. Journal of Archaeological Science 41 (2014) 242-250. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24375,NA,45274,NA,125.968553459119,60.1132075471698,3599.2,NA,65.5454545454545,21,61.1661538461538,40.0861538461538,8.00747663551402,116.689230769231,6.6398753894081,NA,NA,1214.42857142857,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,520,NA,886,NA,591.158513014657,66.89696961967,4331.24420901406,NA,6.44541842275471,2,52.230252092428,42.0395565799639,13.1924883375115,57.2847331196476,17.5693743692769,NA,NA,96.9189646781563,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,325
"ITL011","ITL011","Eurasia","Mediterranean","Italy","Sardinia","Sardinia","Sardinia-D","","5.3-2.6",12.8,"","Active","Intraplate","Continental","Active Continental Margin",39.792,8.665,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: C2 Type (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Terradas, Xavier, Bernard Gratuze, Josep Bosch, Roser Enrich, Xavier Esteve, F. Xavier Oms, Genís Ribé. Neolithic Diffusion of Obsidian in the Western Mediterranean: New Data from Iberia. Journal of Archaeological Science 41 (2014) 69-78. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,88,49,2923,NA,NA,NA,65,35,7.2,97,5.2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.65646419831147,4.16383301038977,449.616859640952,NA,NA,NA,6.28393843870842,7.4784184362429,0.889631590225058,11.0825061161714,0.725383314920616,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,311
"ITL012","ITL012","Eurasia","Mediterranean","Italy","Sardinia","Monte Arci","Monte Arci - Punta Nigola Pani","","5.3-2.6",12.8,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Barca, Donatella, Anna Maria de Francesco, Gino Mirocle Crisci. Application of Laser Ablation ICP-MS for Characterisation of Obsidian Fragments from Peri-Tyrrhenian Area. Journal of Cultural Heritage 8 (2007) 141-150. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,251.625,34.25,19.5,99.5,27.125,NA,7.325,203,29.5,64.5,NA,NA,NA,NA,0.42,NA,NA,NA,NA,29.75,18.75,5.8875,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31.5184186514126,7.40173724781651,1.77281052085584,5.09901951359278,3.04431554587515,NA,0.811964108988639,53.0794552668786,2.39045721866879,2.97609523657138,NA,NA,NA,NA,0.0705083581671604,NA,NA,NA,NA,2.81577190634672,1.38873014965883,0.65123509031466,8
"ITL013","ITL013","Eurasia","Mediterranean","Italy","Sicily","Lipari","Lipari - LIP1","","8-0",4,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",38.494,14.937,"","","","","Obsidian","""Lipari glass is high quality, transparent, and black (Barca et al 2007).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Peccerillo, Angelo. Plio-Quaternary Magmatism in Italy. Episodes 26, 3 (2003) 222-226. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,21,104,3113,NA,NA,NA,105,4.5,16,103,10,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.395292592778873,8.83752312409257,478.842724619324,NA,NA,NA,10.1509774779136,0.961510941802658,1.97695908938902,11.7680219584088,1.39496791330888,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"ITL014","ITL014","Eurasia","Mediterranean","Italy","Sicily","Lipari","Lipari - LST1","","8-0",4,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",38.494,14.937,"","","","","Obsidian","""Lipari glass is high quality, transparent, and black (Barca et al 2007).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Peccerillo, Angelo. Plio-Quaternary Magmatism in Italy. Episodes 26, 3 (2003) 222-226. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23,109,3200,NA,NA,NA,106,5,16,97,10,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.432939506376861,9.2624040435201,492.225094372578,NA,NA,NA,10.2476534538937,1.06834549089184,1.97695908938902,11.0825061161714,1.39496791330888,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"ITL015","ITL015","Eurasia","Mediterranean","Italy","Sicily","Pantelleria","Pantelleria - Balata dei Turchi","","0.3-0.005",0.1525,"Shield","Active","Convergent","Continental","Active Continental Margin",36.784,12.009,"","","","","Obsidian","""Pantelleria obsidian is green, contains microlites, and is common on its island namesake. Subsources are distinguished by their peralkaline character and Zr content (Barca et al 2007).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Peccerillo, Angelo. Plio-Quaternary Magmatism in Italy. Episodes 26, 3 (2003) 222-226. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,177,11,199,1720,339,NA,NA,80,256,468,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2,4,5,21,16,NA,NA,18,5,62.6134961606745,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"ITL016","ITL016","Eurasia","Mediterranean","Italy","Sicily","Pantelleria","Pantelleria - Lago di Venere","","0.3-0.005",0.1525,"Shield","Active","Convergent","Continental","Active Continental Margin",36.784,12.009,"","","","","Obsidian","""Pantelleria obsidian is green, contains microlites, and is common on its island namesake. Subsources are distinguished by their peralkaline character and Zr content (Barca et al 2007).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Peccerillo, Angelo. Plio-Quaternary Magmatism in Italy. Episodes 26, 3 (2003) 222-226. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,126,6,127,1207,223,NA,NA,74,163,299,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,8,1.28201458907021,4,138,7,NA,NA,23,23,40.0030669915421,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"ITL017","ITL017","Eurasia","Mediterranean","Italy","Sicily","Pantelleria","Pantelleria - Salto la Vecchia","","0.3-0.005",0.1525,"Shield","Active","Convergent","Continental","Active Continental Margin",36.784,12.009,"","","","","Obsidian","""Pantelleria obsidian is green, contains microlites, and is common on its island namesake. Subsources are distinguished by their peralkaline character and Zr content (Barca et al 2007).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Peccerillo, Angelo. Plio-Quaternary Magmatism in Italy. Episodes 26, 3 (2003) 222-226. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,156,6,167,1467,280,NA,NA,69,230,413,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,15,1.28201458907021,14,140,33,NA,NA,4,18,55.2550724665782,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"ITL018","ITL018","Eurasia","Mediterranean","Italy","Sardinia","Monte Arci","Monte Arci - Santa Maria Zuarbara","","5.3-2.6",3.95,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; De Francesco, A. M., G. M. Crisci, and M. Bocci. Non-Destructive Analytical Method Using XRF for Determination of Provenance of Archaeological Obsidians from the Mediterranean Area: A Comparison with Traditional XRF Methods. Archaeometry 50, 2 (2008) 337-350. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,245.333333333333,58.6666666666667,27,128,40,NA,NA,224.666666666667,33.6666666666667,70.3333333333333,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.18688672392661,14.8994949366117,5.0153138486728,11.409307353786,7.80330085889911,NA,NA,51.5066918773212,2.91421356237309,5.65685424949238,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9
"ITL019","ITL019","Eurasia","Mediterranean","Italy","Sardinia","Sardinia","Sardinia-B2","","5.3-2.6",3.95,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","""There are two subsources, Sardinia B1 and Sardinia B2 (Terradas et al 2014).""","","""Literature suggests alternate names for this source include: SB Type (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Terradas, Xavier, Bernard Gratuze, Josep Bosch, Roser Enrich, Xavier Esteve, F. Xavier Oms, Genís Ribé. Neolithic Diffusion of Obsidian in the Western Mediterranean: New Data from Iberia. Journal of Archaeological Science 41 (2014) 69-78. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23950,NA,43744,NA,59.8769716088328,55.1514195583596,2873.98493975904,NA,50.4090909090909,19,81.0753012048193,14.9939759036145,7.69846153846154,77.144578313253,6.29230769230769,NA,NA,289.733333333333,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,864,NA,1669,NA,309.204887836564,72.4680374315355,3359.76565737746,NA,5.07013071656114,2,66.3911278250138,14.7697451731833,12.1568720207596,24.1753528457775,16.6373453961157,NA,NA,83.1766336235867,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,332
"ITL020","ITL020","Eurasia","Mediterranean","Italy","Sardinia","Sardinia","Sardinia B Group General","","5.3-2.6",3.95,"","Active","Intraplate","Continental","Active Continental Margin",39.779,8.705,"","","","","Obsidian","""There are two subsources, Sardinia B1 and Sardinia B2 (Terradas et al 2014).""","","""Literature suggests alternate names for this source include: SB Type (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Terradas, Xavier, Bernard Gratuze, Josep Bosch, Roser Enrich, Xavier Esteve, F. Xavier Oms, Genís Ribé. Neolithic Diffusion of Obsidian in the Western Mediterranean: New Data from Iberia. Journal of Archaeological Science 41 (2014) 69-78. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Lustrino, Michele, Leone Melluso, and Vincenzo Morra. The Role of Lower Continental Crust and Lithospheric Mantle in the Genesis of Plio-Pleistocene Volcanic Rocks from Sardinia (Italy). Earth and Planetary Science Letters 180 (2000) 259-270.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,61.4991869918699,53.5024390243902,2642.23577235772,NA,NA,NA,66.5056910569106,20.5008130081301,5.65154471544715,78.5105691056911,6.95170731707317,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.707106781186548,2.12132034355964,205.060966544099,NA,NA,NA,4.94974746830583,0.707106781186548,1.34350288425444,9.19238815542512,1.48492424049175,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,615
"JPN035","JPN035","Eurasia","Japan","Japan","Hokkaido","Oketo","Oketo Group General","","23",23,"","Active","Convergent","Continental","Mature Island Arc",43.41,143.32,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Okedo (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27947.3684210526,NA,34094.7368421053,NA,3312,397.535714285714,10726.4745762712,NA,39.6785714285714,25.55,128.762711864407,84.3677966101695,23.425,139.491525423729,13.6666666666667,NA,NA,1898.96,22.2210526315789,32.706,NA,NA,NA,NA,0.368947368421053,NA,NA,NA,NA,NA,14.928813559322,3.37105263157895,514.639486601631,NA,1927.13768296995,NA,414,76.6998478586209,2145.5886300733,NA,8.73449455650333,5.54534836894126,7.14813439117334,13.5455136833313,2.64573219826396,16.0167979294018,0.555341801261479,NA,NA,563.629594805858,0.417105032560307,7.49888460579914,NA,NA,NA,NA,0.0104853002087607,NA,NA,NA,NA,NA,2.68925406316258,0.232328664153037,59
"JPN043","JPN043","Eurasia","Japan","Japan","Hokkaido","Rubeshibe","Rubeshibe Group General","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.313,143.498,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,710,15310,NA,79,37,119.5,105,31.5,117.5,14,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20,NA,NA,NA,NA,NA,NA,28.0134559672906,722.401153701776,NA,1.70710678118655,1.45710678118655,5.18198051533946,7.90685424949238,0.653553390593274,5.63908729652601,0.65,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.35,NA,6
"JPN049","JPN049","Eurasia","Japan","Japan","Hokkaido","Shirataki","Shirataki Group General","","23",23,"","Active","Convergent","Continental","Mature Island Arc",43.56,143.08,"","","","","Obsidian","""There are six geochemically unique subsources in the Shirataki group (Watanabe and Suzuki 2009).""","","""Literature suggests alternate names for this source include: Akaishshiyama (Hall and Kumura 2002).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3121.29508196721,NA,11110.0655737705,NA,NA,26,186.524590163934,31.5081967213115,31.016393442623,90.016393442623,NA,NA,NA,2868.80327868852,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,18.4918032786885,NA,NA,NA,NA,NA,244.53238380558,NA,228.468954442739,NA,NA,6.50819672131148,4.31475853243556,1.35355339059327,1.46120514184229,2.46120514184229,NA,NA,NA,97.9279043250582,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.35355339059327,NA,61
"JPN055","JPN055","Eurasia","Japan","Japan","Hokkaido","Tokachi","Tokachi Group General","","23",23,"","Active","Convergent","Continental","Mature Island Arc",43.324,143.084,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is Tokachiishikawa, Mitsumata (Hall and Kumura 2002).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29950,NA,35550,NA,3054,519.375,10490.3571428571,NA,57.75,28.0769230769231,187,17.8857142857143,35.9615384615385,81,13.5,NA,NA,1106,22.35,49.7363636363636,NA,NA,NA,NA,0.485,NA,NA,NA,NA,NA,18.325,3.235,353.553390593274,NA,353.553390593274,NA,819,64.1597791901462,1258.86732302409,NA,8.89407078602875,5.93435914300175,30.3116029865069,22.716462266176,2.88941140348438,8.25402913701671,0.628553390593274,NA,NA,211.979638004817,0.0707106781186533,4.5186672306643,NA,NA,NA,NA,0.00707106781186548,NA,NA,NA,NA,NA,2.98438000292099,0.0212132034355963,28
"JPN083","JPN083","Eurasia","Japan","Japan","Hokkaido","Asahikawa","Asahikawa-Higashitakasu","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.778,142.269,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,810,16680,NA,81,35,114,128,28,107,13,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20,NA,NA,NA,NA,NA,NA,49,1063,NA,9,2,5,5,1,0.3,0.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1,NA,3
"JPN084","JPN084","Eurasia","Japan","Japan","Hokkaido","Asahikawa","Asahikawa-Syunkodai","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.778,142.269,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,736,12930,NA,75,37,122,95,29,93,13,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,22,NA,NA,NA,NA,NA,NA,92,959,NA,2,2,6,4,2,2,0.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1,NA,3
"JPN085","JPN085","Eurasia","Japan","Japan","Kanagawa","Hakone","Hakone I","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",35.245,139.079,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,38300,NA,NA,NA,NA,NA,34200,NA,130,NA,11.3,NA,NA,40.5,NA,1.02,1.31,449,6.16,12.8,14.3,0.857,NA,3.75,1.45,3.74,0.564,3.16,0.163,NA,0.577,0.304,2400,NA,NA,NA,NA,NA,2700,NA,11,NA,4.6,NA,NA,38.9,NA,0.09,0.23,54,0.37,1,3.9,0.134,NA,0.23,0.14,0.365295444169159,0.036,0.23,0.17,NA,0.085,0.141,40
"JPN086","JPN086","Eurasia","Japan","Japan","Kanagawa","Hakone","Hakone II","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",35.245,139.079,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36400,NA,NA,NA,NA,NA,18300,NA,87,NA,21.3,NA,NA,102,NA,0.839,2.32,648,8.47,20.7,16.4,0.966,NA,4.56,1.21,4.56,0.695,4.81,0.147,NA,1.15,0.504,2300,NA,NA,NA,NA,NA,2400,NA,10.5,NA,5.1,NA,NA,51,NA,0.08,0.28,62,0.58,1.6,4.2,0.119,NA,0.24,0.14,0.22,0.036,0.34,0.133,NA,0.11,0.228,50
"JPN087","JPN087","Eurasia","Japan","Japan","Oita","Himeshima","Himeshima I","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",33.73,131.671,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,38500,NA,NA,NA,NA,NA,7760,NA,50.5,NA,88.8,NA,NA,40.7,NA,0.345,2.52,1055,9.4,18.4,9.65,0.364,NA,2.47,0.175,0.657,0.105,1.8,1.55,NA,2.17,1.95,8400,NA,NA,NA,NA,NA,230,NA,7.8,NA,5.95,NA,NA,34.1,NA,0.076,0.19,50,8.07,15.6,8.22,0.097,NA,1.06,0.075,0.0641708841762399,0.021,0.4,0.23,NA,1.83,0.16,61
"JPN088","JPN088","Eurasia","Japan","Japan","Oita","Himeshima","Himeshima II","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",33.73,131.671,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33700,NA,NA,NA,NA,NA,11100,NA,51.8,NA,68,NA,NA,54.9,NA,0.399,2.2,954,10,19.7,10.9,0.348,NA,2.46,0.417,0.787,0.127,2.22,1.32,NA,2.1,1.5,1600,NA,NA,NA,NA,NA,1000,NA,6.5,NA,6.4,NA,NA,35.9,NA,0.119,0.18,51,0.6,1.3,2.9,0.099,NA,0.16,0.094,0.082,0.016,0.28,0.24,NA,0.13,0.16,32
"JPN089","JPN089","Eurasia","Japan","Japan","Hokkaido","Ikutahara","Ikutahara-1","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.689,143.556,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,467,13740,NA,81,35,159,48,43,201,13,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,21,NA,NA,NA,NA,NA,NA,18,527,NA,5,5,7,1,0.2,12,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4,NA,3
"JPN090","JPN090","Eurasia","Japan","Japan","Hokkaido","Ikutahara","Ikutahara-2","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.689,143.556,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,173,14760,NA,87,41,161,50,16,205,15,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25,NA,NA,NA,NA,NA,NA,14,52,NA,4,1,1,1,1,2,0.3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1,NA,3
"JPN091","JPN091","Eurasia","Japan","Japan","Tokyo","Kouzushima","Kouzushima I","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",34.425,139.285,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31100,NA,NA,NA,NA,NA,5060,NA,25.3,NA,69.2,NA,NA,63.8,NA,0.157,2.52,753,19.9,37.9,17.3,0.55,NA,3.18,0.475,2.85,0.445,2.56,0.787,NA,5.05,1.75,1300,NA,NA,NA,NA,NA,660,NA,11.7,NA,7.4,NA,NA,45.9,NA,0.05,0.3,48,0.9,2.5,6.1,0.164,NA,0.15,0.147,0.18,0.027,0.33,0.271,NA,0.28,0.22,40
"JPN092","JPN092","Eurasia","Japan","Japan","Tokyo","Kouzushima","Kouzushima II","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",34.425,139.285,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31500,NA,NA,NA,NA,NA,5270,NA,26.7,NA,63.3,NA,NA,58.8,NA,0.156,2.3,731,19.9,37.7,16,0.561,NA,3.19,0.511,2.82,0.434,2.78,0.607,NA,4.76,1.69,1900,NA,NA,NA,NA,NA,410,NA,9.9,NA,6.5,NA,NA,45.8,NA,0.04,0.31,49,0.9,2.3,5.9,0.134,NA,0.305104823244473,0.141,0.12,0.200148537850162,0.21,0.208,NA,0.27,0.2,90
"JPN093","JPN093","Eurasia","Japan","Japan","Tokyo","Kouzushima","Kouzushima III","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",34.425,139.285,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33200,NA,NA,NA,NA,NA,5800,NA,35.4,NA,68.9,NA,NA,73.1,NA,0.42,2.41,761,20.8,38.5,20.5,0.575,NA,3.38,0.622,2.85,0.46,2.84,0.62,NA,4.92,1.75,900,NA,NA,NA,NA,NA,220,NA,7.2,NA,4.8,NA,NA,31.3,NA,0.035,0.22,43,0.6,1.6,3.5,0.111,NA,0.1,0.113,0.08,0.02,0.42,0.253,NA,0.19,0.21,62
"JPN094","JPN094","Eurasia","Japan","Japan","Tokyo","Kouzushima","Kouzushima IV","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",34.425,139.285,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30900,NA,NA,NA,NA,NA,9940,NA,47.2,NA,47.2,NA,NA,48.9,NA,0.611,2.28,659,14.3,30.4,19.4,0.692,NA,3.58,0.878,3.34,0.523,3.53,0.395,NA,3.2,1.21,5600,NA,NA,NA,NA,NA,5430,NA,22.3,NA,23.1,NA,NA,40.8,NA,0.235,0.27,60,5.4,8.5,4.1,0.222,NA,0.342406039879378,0.120572774670564,0.84,0.11,0.91,0.254,NA,1.72,0.52,10
"JPN095","JPN095","Eurasia","Japan","Japan","Hokkaido","Oketo","Oketo I","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.41,143.32,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Oketo, Oketo A, Oketo 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28673.4513274336,NA,34700,NA,NA,303.63829787234,7691.60544217687,NA,33.0816326530612,15,137.040816326531,66.0425531914894,25,94.2585034013605,3,0.471,6.96,1290.84955752212,24.6663716814159,44.8274336283186,18.6,0.541,NA,3.32,0.399513274336283,2.66,0.463,3.42,0.607,NA,12.1816326530612,3.85663716814159,1125.63439336942,NA,1900,NA,NA,35.2406005231747,275.795993999814,NA,5.90007842808583,1,5.94942364683959,6.77206601993027,1,18.1563036788274,1,0.0352750673024324,0.56,170.443230662185,1.83902164687979,2.24625928942973,3.3,0.103,NA,0.27,0.0552266353304828,0.17,0.029,0.21,0.174,NA,1.94023892057241,0.255627828404793,147
"JPN096","JPN096","Eurasia","Japan","Japan","Hokkaido","Oketo","Oketo II","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.41,143.32,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Oketo, Oketo B, Oketo 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32432.0754716981,NA,28400,NA,NA,356.5,9442.2037037037,NA,38.8888888888889,14,101.592592592593,85.5,21,111.074074074074,2,0.566,5.54,933.981132075472,23.5528301886792,42.3716981132075,18.9,0.503,NA,3.25,0.577339622641509,2.58,0.434,3.85,0.541,NA,10.0722222222222,2.76037735849057,1160.1131253157,NA,9100,NA,NA,26.6310966544099,374.566688078975,NA,4.89536037070996,2,5.45570734307187,13.8247474683058,1,25.3471466936504,1,0.109,0.38,118.751242100604,1.49093692875006,1.32583329907022,4,0.109,NA,0.16,0.0688717263390159,0.13,0.024,0.27,0.217,NA,1.06080841502057,0.174255019797083,108
"JPN097","JPN097","Eurasia","Japan","Japan","Hokkaido","Oketo","Oketo III","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.41,143.32,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Oketo (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31100,NA,NA,NA,NA,NA,9170,NA,48.6,NA,96.5,NA,NA,103,NA,0.573,5.27,879,22.3,39.3,17.6,0.511,NA,3.08,0.533,2.43,0.404,3.67,0.497,NA,9.36,2.58,1500,NA,NA,NA,NA,NA,660,NA,12.9,NA,11,NA,NA,35,NA,0.11,0.56,78,1.6,3.9,3.5,0.111,NA,0.2,0.099,0.21,0.186313385464206,0.38,0.0482115281058525,NA,0.85,0.3,100
"JPN098","JPN098","Eurasia","Japan","Japan","Hokkaido","Oketo","Oketo IV","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.41,143.32,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Oketo (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32800,NA,NA,NA,NA,NA,9780,NA,40.9,NA,102,NA,NA,112,NA,0.627,5.69,979,23.9,44.2,18.5,0.544,NA,3.37,0.598,2.65,0.437,4.04,0.518,NA,10.4,2.7,2300,NA,NA,NA,NA,NA,920,NA,14.1,NA,12,NA,NA,35,NA,0.112,0.35,55,1.9,2.6,3.7,0.08,NA,0.16,0.123,0.13,0.201532053088757,0.4,0.207,NA,0.6,0.21,100
"JPN099","JPN099","Eurasia","Japan","Japan","Hokkaido","Oketo","Oketo V","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.41,143.32,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Oketo (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28300,NA,NA,NA,NA,NA,7600,NA,29.7,NA,141,NA,NA,91.8,NA,0.579,6.95,1319,24.8,44.3,19.2,0.507,NA,3.3,0.381,2.67,0.453,3.37,0.59,NA,13,3.88,1600,NA,NA,NA,NA,NA,430,NA,6.2,NA,11,NA,NA,34,NA,0.037,0.41,87,1.4,2.4,3.1,0.086,NA,0.18,0.089,0.17,0.208910801027934,0.19,0.16,NA,0.7,0.36,100
"JPN101","JPN101","Eurasia","Japan","Japan","Shimane","Oki","Oki I","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",36.296,133.244,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31100,NA,NA,NA,NA,NA,14100,NA,81.4,NA,205,NA,NA,324,NA,0.628,2.04,32.3,118,206,88.9,1.63,NA,12.7,0.0552,4.57,0.693,13.6,4.87,NA,28.5,4.09,1000,NA,NA,NA,NA,NA,500,NA,6.8,NA,8,NA,NA,39,NA,0.032,0.19,24.8,5,8,7.3,0.219894790529426,NA,0.5,0.00758042956926553,0.21,0.027,0.8,0.37,NA,1.1,0.35,28
"JPN102","JPN102","Eurasia","Japan","Japan","Shimane","Oki","Oki II","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",36.296,133.244,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29900,NA,NA,NA,NA,NA,13500,NA,78.5,NA,199,NA,NA,308,NA,0.533,2.02,21.7,111,189,81.7,1.58,NA,12,0.0352,4.53,0.68,12.3,4.77,NA,27,3.89,1200,NA,NA,NA,NA,NA,600,NA,6.1,NA,11,NA,NA,50,NA,0.139,0.18,25.2,4,9,6.5,0.14,NA,0.4,0.057,0.21,0.029,0.8,0.35,NA,1.3,0.28,16
"JPN103","JPN103","Eurasia","Japan","Japan","Shimane","Oki","Oki III","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",36.296,133.244,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33100,NA,NA,NA,NA,NA,15200,NA,80.5,NA,211,NA,NA,393,NA,0.623,2.31,33.4,114,207,77.8,1.53,NA,12.4,0.062,4.49,0.714,13.3,4.4,NA,29,4.07,1100,NA,NA,NA,NA,NA,600,NA,13,NA,13,NA,NA,53,NA,0.041,0.24,31.8,12,23,8.88,0.26,NA,1.5,0.0838,0.53,0.075,1.1,0.49,NA,2.2,0.33,10
"JPN104","JPN104","Eurasia","Japan","Japan","Shimane","Oki","Oki IV","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",36.296,133.244,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33800,NA,NA,NA,NA,NA,14300,NA,115,NA,219,NA,NA,416,NA,0.537,2.49,38.4,94,175,79.5,1.93,NA,13.9,0.037,5.65,0.837,16.8,6.24,NA,28,4.59,2000,NA,NA,NA,NA,NA,900,NA,6,NA,17,NA,NA,49,NA,0.074,0.26,22.4,4.2,10,6,0.260366224369197,NA,0.8,0.0459,0.3,0.048,1.3,0.34,NA,1.7,0.29,19
"JPN105","JPN105","Eurasia","Japan","Japan","Shimane","Oki","Oki V","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",36.296,133.244,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31000,NA,NA,NA,NA,NA,13400,NA,77.2,NA,211,NA,NA,272,NA,0.623,2.23,30.7,113,193,79,1.56,NA,12.3,0.036,4.47,0.687,12.4,4.52,NA,28.7,4.14,1200,NA,NA,NA,NA,NA,500,NA,7.6,NA,10,NA,NA,41,NA,0.059,0.2,28.6,4,9,4.5,0.14,NA,0.5,0.05,0.21,0.024,0.5,0.34,NA,1.4,0.54,35
"JPN106","JPN106","Eurasia","Japan","Japan","Shimane","Oki","Oki VI","","2.6-0",1.3,"","Active","Convergent","Continental","Mature Island Arc",36.296,133.244,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31800,NA,NA,NA,NA,NA,14000,NA,54.4,NA,181,NA,NA,258,NA,0.632,1.77,68.7,84.2,145,57.7,0.937,NA,8.53,0.248,3.14,0.496,11.3,3.41,NA,24.9,4.4,1000,NA,NA,NA,NA,NA,500,NA,3.3,NA,6,NA,NA,25,NA,0.03,0.13,14.9,2.3,3,3.9,0.11,NA,0.21,0.0340570024126422,0.1,0.22874118611447,0.3,0.330787345756453,NA,0.7,0.26,30
"JPN107","JPN107","Eurasia","Japan","Japan","Nagano","Omegura","Omegura I","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27600,NA,NA,NA,NA,NA,6310,NA,32.1,NA,161,NA,NA,117,NA,0.686,9.97,391,26.1,52.6,26.2,0.596,NA,4.66,0.524,2.71,0.487,4.68,0.819,NA,17.8,5,2900,NA,NA,NA,NA,NA,810,NA,16.7,NA,18,NA,NA,74,NA,0.136,1.06,84,2.2,7.03732884199034,3.56669926739712,0.172,NA,0.4,0.276,0.27,0.047,0.53,0.079447166033588,NA,1.5,0.58,104
"JPN108","JPN108","Eurasia","Japan","Japan","Nagano","Omegura","Omegura II","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28700,NA,NA,NA,NA,NA,6860,NA,37.5,NA,141,NA,NA,137,NA,0.578,8.09,569,25.5,51.3,26.7,0.573,NA,4.54,0.702,2.57,0.448,5.15,0.691,NA,14.6,4.1,3800,NA,NA,NA,NA,NA,1540,NA,16,NA,22,NA,NA,77,NA,0.13,1.25,92,3,5.9,3.63476604730928,0.186,NA,0.54,0.23,0.38,0.062,0.65,0.324,NA,1.62193649486966,0.62,104
"JPN109","JPN109","Eurasia","Japan","Japan","Nagano","Omegura","Omegura II","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28500,NA,NA,NA,NA,NA,6470,NA,35.3,NA,156,NA,NA,119,NA,0.684,9.55,425,25.9,52.2,25.8,0.565,NA,4.64,0.576,2.67,0.475,4.79,0.74,NA,17.3,4.83,2200,NA,NA,NA,NA,NA,810,NA,18.1,NA,18,NA,NA,71,NA,0.147,1.29,91,1.8,4.2,3.5122458434674,0.161,NA,0.34,0.217,0.26,0.047,0.51,0.312,NA,2.1,0.62,104
"JPN110","JPN110","Eurasia","Japan","Japan","Nagano","Omegura","Omegura IV","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27900,NA,NA,NA,NA,NA,6160,NA,32.5,NA,165,NA,NA,114,NA,0.729,10.5,355,25.7,52.3,26.4,0.589,NA,4.66,0.503,2.77,0.49,4.64,0.881,NA,18.6,5.16,2500,NA,NA,NA,NA,NA,780,NA,13.4,NA,26,NA,NA,66,NA,0.192,1.9,91,2.20985804199734,4.9,6.4,0.165,NA,0.45,0.213,0.34,0.062,0.53,0.326,NA,2.7,0.82,104
"JPN111","JPN111","Eurasia","Japan","Japan","Nagano","Wada","Wada I","","",NA,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29900,NA,NA,NA,NA,NA,5270,NA,36.4,NA,260,NA,NA,118,NA,1.47,21.3,79.9,22,50.5,27.2,0.968,NA,6.27,0.281,4.79,0.839,5.06,1.61,NA,28.1,9.23,1700,NA,NA,NA,NA,NA,740,NA,19,NA,22,NA,NA,80,NA,0.27,1.81076622220104,43.5,1.1,3,3.70283282722144,0.157,NA,0.31,0.154,0.37,0.052,0.503625487936677,0.156178189638677,NA,1.5,0.72,104
"JPN112","JPN112","Eurasia","Japan","Japan","Nagano","Wada","Wada II","","",NA,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28800,NA,NA,NA,NA,NA,4610,NA,36.4,NA,267,NA,NA,114,NA,1.52,22,67.2,21.7,50.1,27.4,1,NA,6.31,0.246,4.88,0.855,5.18,1.71,NA,28.9,9.47,1800,NA,NA,NA,NA,NA,360,NA,15.6,NA,22,NA,NA,62,NA,0.26,1.5,34.8,1.86591126503277,6.70285503771323,7.5,0.16,NA,0.603514556323708,0.143,0.36,0.057,0.515569175397626,0.31,NA,1.5,0.7,104
"JPN114","JPN114","Eurasia","Japan","Japan","Hokkaido","Shirataki","Shirataki I","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.56,143.08,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Shirataki A, Akaishshiyama (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473. ; Glascock, Michael D, Yaroslav V. Kuzmin, Andrei V. Grebennikov, Vladmir ; K. Popov, Vitaly E. Medvedev, Igor Y. Shrewkomud, and Nikolai N. Zaitsev. Obsidian Provenance for Prehistoric Complexes in the Amur River Basin Russia Far East). Journal of Archaeological Science 38 2011) 1832-1841. ; Kimura, Hideaki and Evgeny Girya. Human Activity Patterns at the Horokazawa Toma Upper Stone Tool Manufacturing Site in the Shirataki Obsidian Source Area: Combining Excavation with Experimentation. Quaternary International 397 2016) 448-473. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Philips, S Colby and Robert J. Speakman. Initial Source Evaluation of Archaeological Obsidian from the Kuril Islands of the Russian Far East using Portable XRF. Journal of Archaeological Science 39 2009) 1256-1263. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29449.6644295302,NA,37932.6530612245,NA,NA,398.983606557377,7872.4498265896,NA,41.7530120481928,22.7058823529412,157.872832369942,25.5878787878788,28.8823529411765,80.4277108433735,8.25,0.607,10.5,1058.47435897436,22.3064102564103,45.7846153846154,20.5,0.73,NA,4.27,0.312576923076923,3.29,0.529,3.17,0.594,NA,12.3105590062112,3.52864864864865,2867.66646269503,NA,1879.49470513913,NA,NA,45.4124499981577,2113.27881617328,NA,22.5973942400756,5.82581315052319,12.6666132685525,6.57321256007447,2.50122209206585,26.5708981664312,3.82791225845875,0.07,1.2,142.513452204923,5.17528288326812,8.21018534659638,8.5,0.338,NA,2.13,0.155794300739589,1.15,0.142,2.03,0.553,NA,1.58755516769003,0.352100310473281,173
"JPN115","JPN115","Eurasia","Japan","Japan","Hokkaido","Shirataki","Shirataki II","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.56,143.08,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Shirataki B, Akaishshiyama (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Kimura, Hideaki and Evgeny Girya. Human Activity Patterns at the Horokazawa Toma Upper Stone Tool Manufacturing Site in the Shirataki Obsidian Source Area: Combining Excavation with Experimentation. Quaternary International 397 2016) 448-473. ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Philips, S Colby and Robert J. Speakman. Initial Source Evaluation of Archaeological Obsidian from the Kuril Islands of the Russian Far East using Portable XRF. Journal of Archaeological Science 39 2009) 1256-1263. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29016.1290322581,NA,38345.8333333333,NA,NA,466.27027027027,8020.78985507246,NA,39.1751824817518,24.2307692307692,156.710144927536,4.54054054054054,34.1538461538462,73.5547445255474,9.07692307692308,0.565,9.69,941.488,20.3552,40.9016,19.1,0.674,NA,3.85,0.2464,2.98,0.483,2.9,0.584,NA,11.5656934306569,3.57656,971.517905660327,NA,1752.50855401167,NA,NA,71.2156751832501,498.717100794508,NA,10.4069304157489,6.91688947919748,12.163810648421,5.08429736511132,2.06303572126476,19.6089855205481,4.02928921355861,0.035,0.63,354.619574332459,3.51588659636433,5.2150801673192,2.8,0.089,NA,0.16,0.0923079771436884,0.16,0.02,0.18,0.181,NA,2.04947626362285,0.214915987288007,138
"JPN116","JPN116","Eurasia","Japan","Japan","Hokkaido","Shirataki","Shirataki III","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.56,143.08,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Akaishshiyama (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30700,NA,NA,NA,NA,NA,8770,NA,36.9,NA,173,NA,NA,67.4,NA,0.612,10.4,1170,23.6,47.6,18.7,0.641,NA,4.21,0.298,3.27,0.525,3.13,0.529,NA,13.1,3.74,2800,NA,NA,NA,NA,NA,820,NA,7.5,NA,18,NA,NA,34.7,NA,0.063,0.884129986426801,104,2.4,6.36838123343613,3.3,0.094,NA,0.47,0.095,0.32,0.054,0.36,0.21,NA,1.45529918375291,0.443673458637434,99
"JPN117","JPN117","Eurasia","Japan","Japan","Hokkaido","Shirataki","Shirataki IV","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.56,143.08,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Akaishshiyama (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29700,NA,NA,NA,NA,NA,8350,NA,37.6,NA,160,NA,NA,67.1,NA,0.573,10.1,1185,22.5,43.9,18.3,0.657,NA,3.91,0.314,3.02,0.497,2.96,0.554,NA,12.2,3.66,1300,NA,NA,NA,NA,NA,400,NA,6.8,NA,10,NA,NA,31.6,NA,0.057,0.7,58,1.1,2,2.6,0.079,NA,0.18,0.088,0.12,0.229202357860669,0.19,0.16,NA,0.6,0.27,100
"JPN118","JPN118","Eurasia","Japan","Japan","Hokkaido","Shirataki","Shirataki V","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.56,143.08,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Akaishshiyama (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30600,NA,NA,NA,NA,NA,7930,NA,34.6,NA,182,NA,NA,70.7,NA,0.674,12.6,265,15.2,34.5,15.8,0.767,NA,3.89,0.161,3.71,0.586,2.89,0.666,NA,10.9,4.34,2700,NA,NA,NA,NA,NA,530,NA,7,NA,18,NA,NA,39.2,NA,0.084,1,31,1,2.8,3.6,0.106,NA,0.3,0.076,0.27,0.047,0.22,0.209,NA,0.8,0.54,100
"JPN119","JPN119","Eurasia","Japan","Japan","Hokkaido","Shirataki","Shirataki VI","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.56,143.08,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Akaishshiyama (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29200,NA,NA,NA,NA,NA,7440,NA,36.5,NA,175,NA,NA,66,NA,0.637,11.9,234,14.1,31.3,15.2,0.742,NA,3.63,0.14,3.5,0.558,2.72,0.656,NA,10.1,3.99,1700,NA,NA,NA,NA,NA,500,NA,6.4,NA,14,NA,NA,28.5,NA,0.071,0.9,30,0.8,1.5,3.1,0.102,NA,0.15,0.073,0.17,0.03,0.24,0.0636353368962561,NA,0.5,0.34,100
"JPN120","JPN120","Eurasia","Japan","Japan","Hokkaido","Tokachi","Tokachi I","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.324,143.084,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is Tokachiishikawa I, Mitsumata (Hall and Kumura 2002).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29900,NA,NA,NA,NA,NA,7250,NA,42.2,NA,136,NA,NA,88.7,NA,0.463,8.24,1143,24.3,48.1,26.4,0.792,NA,4.54,0.538,3.33,0.539,3.24,0.639,NA,13,3.98,1400,NA,NA,NA,NA,NA,330,NA,6.7,NA,8,NA,NA,37.3,NA,0.0346759154161915,0.42,62,1.1,2,3.9,0.108,NA,0.21,0.12,0.325249686920668,0.026,0.322479561445619,0.255,NA,0.6,0.47214448272112,80
"JPN121","JPN121","Eurasia","Japan","Japan","Hokkaido","Tokachi","Tokachi II","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",43.324,143.084,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is Tokachiishikawa II, Mitsumata (Hall and Kumura 2002).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Kuzmin, Yaroslav V., Michael D. Glascock, and Hiroyuki Sato. Sources of Archaeological Obsidian on Sakhalin Island Russia Far East). Journal of Archaeological Science 29 2002) 741-749. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016. ; Hall, Mark and Hideaki Kimura. Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido. Journal of Archaeological Science 2002) 29, 259-266. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30600,NA,NA,NA,NA,NA,7820,NA,40.9,NA,155,NA,NA,95,NA,0.614,8.9,1181,25,50.3,24.9,0.77,NA,4.73,0.555,3.46,0.567,3.5,0.629,NA,13.7,4.08,3600,NA,NA,NA,NA,NA,1020,NA,7.3,NA,12,NA,NA,50.6,NA,0.087,0.39,61,1.5,2.9,4.5,0.144,NA,0.27,0.115,0.22,0.05,0.75,0.274,NA,0.7,0.41,68
"JPN122","JPN122","Eurasia","Japan","Japan","Hokkaido","Rubeshibe","Rubeshibe I","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.313,143.498,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30500,NA,NA,NA,NA,NA,12500,NA,45.6,NA,129,NA,NA,91.5,NA,0.527,8.08,968,23.5,47.1,20.9,0.603,NA,4.17,0.598,2.79,0.452,3.85,0.576,NA,10.5,3.18,2500,NA,NA,NA,NA,NA,800,NA,9.8,NA,16,NA,NA,42.6,NA,0.098,1.68,169,3.9,8.4,5.4,0.151,NA,0.65,0.113,0.42,0.07,0.32,0.308,NA,1.9,0.66,60
"JPN123","JPN123","Eurasia","Japan","Japan","Hokkaido","Rubeshibe","Rubeshibe II","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.313,143.498,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28600,NA,NA,NA,NA,NA,12700,NA,45.4,NA,124,NA,NA,82.1,NA,0.54,6.12,985,25.8,49.1,23.4,0.636,NA,4.16,0.636,2.63,0.438,3.81,0.379,NA,10.3,2.71,900,NA,NA,NA,NA,NA,800,NA,2.4,NA,7,NA,NA,27.8,NA,0.024,0.35,48,1.2,1.9,4.4,0.08,NA,0.19,0.053,0.1,0.02,0.2,0.189,NA,0.4,0.18,8
"RUS007","RUS007","Eurasia","Northeast Asia","Russia","Primorsky Krai","Gladkaya River","Gladkaya River Group General","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",42.799,130.819,"","","","","Obsidian","""There are three unique subsources for Gladkaya obsidian (Kuzmin et al 2002). The use of the Gladkaya glass was rarely used in the Upper Paleolithic, but was used commonly in the Neolithic (Kuzmin 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Jia, Peter Weiming, Trudy Doelman, Chuanjia Chen, Hailong Zhao, Sam Lin, Robin Torrence, and Michael D. Glascock. Moving Sources: A Preliminary Study of Volcanic Glass Artifact Distributions in Northeast China Using pXRF. Journal of Archaeological Science 37 2010) 1670-1677. ; Chen, Yang, Youxue Zhang, David Graham, Shangguo Su, and Jinfu Deng. Geochemistry of Cenozoic Basalts and Mantle Xenoliths in Northeast China. Lithos 96 (2007) 108-126. ; Kuzmin, Yaroslav V. The Patterns of Obsidian Exploitation in the Late Upper Pleistocene of the Russian Far East and Neighboring Northeast Asia. Natural Resource Environment and Humans 1 (2011) 67-82.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30699.68,NA,68460.16,NA,NA,138.42,5185.48,NA,NA,8.04,31.14,22.61,33.67,2.31,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.09,NA,4870.33422749672,NA,2069.62,NA,NA,89.89,2876.76,NA,NA,0.67,18.36,1.39,54.25,37.69,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.9,NA,12
"RUS030","RUS030","Eurasia","Northeast Asia","Russia","Primorsky Krai","Basaltic Plateau","Basaltic Plateau Group General","","",NA,"","Inactive","Convergent","Continental","Active Continental Margin",43.693,132.476,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is the Shoktovo Plateau (Jia et al 2010).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D, Yaroslav V. Kuzmin, Andrei V. Grebennikov, Vladmir K. Popov, Vitaly E. Medvedev, Igor Y. Shrewkomud, and Nikolai N. Zaitsev. Obsidian Provenance for Prehistoric Complexes in the Amur River Basin Russia Far East). Journal of Archaeological Science 38 2011) 1832-1841. ; Kuzmin; Y. V., V. K. Popov, M. D. Glascock, and M. S. Shackley. Sources of Archaeological Volcanic Glass in the Primorye Maritime) Province, Russian Far East. Archaeometry 44, 4 2002) 505-515.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24667.1268531469,NA,6108.17594405594,NA,NA,1097.17944055944,47080.6060927152,NA,129.590277777778,12.6666666666667,11.5296026490066,375.815364238411,75.8573333333333,91.1390066225166,NA,NA,NA,122.713235294118,6.32867647058824,14.3286764705882,NA,NA,NA,NA,1.44147058823529,NA,NA,NA,NA,NA,1.02062937062937,NA,2545.50040715212,NA,7715.50441706348,NA,NA,35.7012218203184,23545.5033356919,NA,15.4762116297663,2.22576695296637,2.19727650790967,103.175977569182,54.927248506855,20.3391820342002,NA,NA,NA,15.2101710376521,0.542561221412269,1.04969357435344,NA,NA,NA,NA,0.049142135623731,NA,NA,NA,NA,NA,0.90779627397513,NA,151
"RUS031","RUS031","Eurasia","Northeast Asia","Russia","Primorsky Krai","Gladkaya River","Gladkaya River 1","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",42.799,130.819,"","","","","Obsidian","""There are three unique subsources for Gladkaya obsidian (Kuzmin et al 2002). The use of the Gladkaya glass was rarely used in the Upper Paleolithic, but was used commonly in the Neolithic (Kuzmin 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Kuzmin; Y. V., V. K. Popov, M. D. Glascock, and M. S. Shackley. Sources of Archaeological Volcanic Glass in the Primorye Maritime) Province, Russian Far East. Archaeometry 44, 4 2002) 505-515. ; Chen, Yang, Youxue Zhang, David Graham, Shangguo Su, and Jinfu Deng. Geochemistry of Cenozoic Basalts and Mantle Xenoliths in Northeast China. Lithos 96 (2007) 108-126.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,26400,NA,36600,NA,NA,223,5300,NA,22.4,NA,97.3,199,NA,106,NA,NA,NA,90,25.7,46.5,NA,NA,NA,NA,0.12,NA,NA,NA,NA,NA,16.6,4.07,500,NA,900,NA,NA,3,200,NA,3.31069082811532,NA,2.1,1.5,NA,10,NA,NA,NA,12,1.4,2.3,NA,NA,NA,NA,0.01,NA,NA,NA,NA,NA,0.4,0.71,6
"RUS032","RUS032","Eurasia","Northeast Asia","Russia","Primorsky Krai","Gladkaya River","Gladkaya River 2","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",42.799,130.819,"","","","","Obsidian","""There are three unique subsources for Gladkaya obsidian (Kuzmin et al 2002). The use of the Gladkaya glass was rarely used in the Upper Paleolithic, but was used commonly in the Neolithic (Kuzmin 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Kuzmin; Y. V., V. K. Popov, M. D. Glascock, and M. S. Shackley. Sources of Archaeological Volcanic Glass in the Primorye Maritime) Province, Russian Far East. Archaeometry 44, 4 2002) 505-515. ; Chen, Yang, Youxue Zhang, David Graham, Shangguo Su, and Jinfu Deng. Geochemistry of Cenozoic Basalts and Mantle Xenoliths in Northeast China. Lithos 96 (2007) 108-126.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29700,NA,23600,NA,NA,381,7800,NA,57,NA,59.3,485,NA,156,NA,NA,NA,926,39.4,69.7,NA,NA,NA,NA,0.67,NA,NA,NA,NA,NA,12.3,1.9,3400,NA,5500,NA,NA,6,100,NA,6,NA,0.1,28,NA,8,NA,NA,NA,14,0.8,0.8,NA,NA,NA,NA,0.02,NA,NA,NA,NA,NA,0.1,0.31,2
"RUS033","RUS033","Eurasia","Northeast Asia","Russia","Primorsky Krai","Gladkaya River","Gladkaya River 3","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",42.799,130.819,"","","","","Obsidian","""There are three unique subsources for Gladkaya obsidian (Kuzmin et al 2002). The use of the Gladkaya glass was rarely used in the Upper Paleolithic, but was used commonly in the Neolithic (Kuzmin 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Kuzmin; Y. V., V. K. Popov, M. D. Glascock, and M. S. Shackley. Sources of Archaeological Volcanic Glass in the Primorye Maritime) Province, Russian Far East. Archaeometry 44, 4 2002) 505-515.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,26700,NA,36800,NA,NA,205,5900,NA,23,NA,89,39,NA,115,NA,NA,NA,262,31.7,53.7,NA,NA,NA,NA,0.212,NA,NA,NA,NA,NA,16.3,3.16,200,NA,800,NA,NA,7,100,NA,3,NA,1,33,NA,2,NA,NA,NA,7,0.3,0.2,NA,NA,NA,NA,0.002,NA,NA,NA,NA,NA,0.1,0.21,2
"RUS034","RUS034","Eurasia","Beringia","Russia","Chukotka Autonomous Okrug","Lake Kraseno","Lake Kraseno 1","","",NA,"","Inactive","Convergent","Continental","Active Continental Margin",64.528,174.83,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Kankaren Mtn., Krasnoy Lake (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Grebennikov, Andrei V., Yaroslav V. Kuzmin, Michael D. Glascock, Vladmir K. Popov, Sergey Y. Budnitskiy, Margarita A. Dikova, and Evgeniy A. Nozdrachev. The Lake Krasnoe Obsidian Source in Chukotka (Northeastern Siberia): Geological and Geochemical Frameworks from Provenance Studies in Beringia. Archaeological Anthropology Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29186.35,NA,39248.05,NA,NA,78.0525,5850.875,NA,57.2115,NA,197.1625,NA,NA,154.9975,NA,NA,NA,33.42025,21.208,55.428,NA,NA,NA,NA,NA,NA,NA,6,NA,NA,15.30675,6.256,406.728720122478,NA,962.508076407728,NA,NA,1.80595170766009,640.672867584466,NA,1.8096799889413,NA,1.5961389808526,NA,NA,6.77020897057511,NA,NA,NA,13.3139988750729,0.351694528400084,0.745193118080377,NA,NA,NA,NA,NA,NA,NA,0.15,NA,NA,0.0967782200565365,0.300185268829077,40
"RUS035","RUS035","Eurasia","Beringia","Russia","Chukotka Autonomous Okrug","Lake Kraseno","Lake Kraseno 2","","",NA,"","Inactive","Convergent","Continental","Active Continental Margin",64.528,174.83,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Kankaren Mtn., Krasnoy Lake (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Grebennikov, Andrei V., Yaroslav V. Kuzmin, Michael D. Glascock, Vladmir K. Popov, Sergey Y. Budnitskiy, Margarita A. Dikova, and Evgeniy A. Nozdrachev. The Lake Krasnoe Obsidian Source in Chukotka (Northeastern Siberia): Geological and Geochemical Frameworks from Provenance Studies in Beringia. Archaeological Anthropology Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31702.1875,NA,37995.375,NA,NA,113.010625,10340.1875,NA,106.240625,NA,141.90125,NA,NA,399.051875,NA,NA,NA,26.9675,37.418125,90.155,NA,NA,NA,NA,NA,NA,NA,13.6,NA,NA,12.20625,4.189375,551.041415148109,NA,1435.12696009127,NA,NA,4.4012838554285,97.783183790099,NA,1.40913200139468,NA,0.818419159080551,NA,NA,15.004988125762,NA,NA,NA,10.828194444498,0.427852146092098,0.821460103773812,NA,NA,NA,NA,NA,NA,NA,0.2,NA,NA,0.0733940720845185,0.248565113106713,16
"RUS036","RUS036","Eurasia","Beringia","Russia","Chukotka Autonomous Okrug","Lake Kraseno","Lake Kraseno 3","","",NA,"","Inactive","Convergent","Continental","Active Continental Margin",64.528,174.83,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Kankaren Mtn., Krasnoy Lake (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Grebennikov, Andrei V., Yaroslav V. Kuzmin, Michael D. Glascock, Vladmir K. Popov, Sergey Y. Budnitskiy, Margarita A. Dikova, and Evgeniy A. Nozdrachev. The Lake Krasnoe Obsidian Source in Chukotka (Northeastern Siberia): Geological and Geochemical Frameworks from Provenance Studies in Beringia. Archaeological Anthropology Science 2016.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36087,NA,33419,NA,NA,378.54,17814,NA,87.68,NA,131.82,NA,NA,428.72,NA,NA,NA,618.5,31.35,72.96,NA,NA,NA,NA,NA,NA,NA,12.2,NA,NA,10.34,3.74,5725.00271233036,NA,4190.49654652354,NA,NA,32.1668846480192,2740.15557223535,NA,12.9589898129086,NA,12.7438271537007,NA,NA,48.98239198067,NA,NA,NA,68.2060232668673,2.69568286445979,9.7612835040231,NA,NA,NA,NA,NA,NA,NA,1.21427489186313,NA,NA,1.1486865312981,0.443673458637434,1
"TKY009","TKY009","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 1","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.254,34.487,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gratuze, B. Obsidian Characterization by Laser Ablation ICP-MS and its Application to Prehistoric Trade in the Mediterranean and the Near East: Sources and Distribution of Obsidian within Aegean and Anatolia. Journal of Archaeological Science (1999) 26, 891-881. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,426,NA,NA,NA,NA,NA,170,30,18,76,23,NA,NA,359,33,55,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25,7.3,NA,NA,NA,NA,23,NA,NA,NA,NA,NA,6,1.3,1.1,4,1.1,NA,NA,13,2,3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.3,0.4,7
"TKY010","TKY010","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 2","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.318,34.48,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gratuze, B. Obsidian Characterization by Laser Ablation ICP-MS and its Application to Prehistoric Trade in the Mediterranean and the Near East: Sources and Distribution of Obsidian within Aegean and Anatolia. Journal of Archaeological Science (1999) 26, 891-881. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,623,NA,NA,NA,NA,NA,175,54,19,121,21,NA,NA,420,37,63,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25,8,NA,NA,NA,NA,12,NA,NA,NA,NA,NA,4,1.4,0.5,3,0.5,NA,NA,6,2,0.3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.4,0.2,4
"TKY011","TKY011","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 7","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.24,34.543,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,310,NA,NA,NA,NA,NA,199,5.6,19,61,27,NA,NA,55,19,38,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,16,9.3,NA,NA,NA,NA,12,NA,NA,NA,NA,NA,5,0.8,1.3,5,1.5,NA,NA,6,2,0.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.2,0.1,5
"TKY023","TKY023","Eurasia","Persian Belt","Turkey","Bitlis","Nemrut Dag","Nemrut Dag I","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.61,42.248,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Lake Van (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khazaee, M., M. D. Glascock, P. Masjedi, F. Khademi Nadoshan, R. Soleimani Farsani, M. Delfan, A. Mansori, B. Sodaie, and A. Dolatyari. Sourcing the Obsidian of Prehistoric Tools Found in Western Iran to Southeast Turkey: A Case Study for the Sites of Eastern Chia Sabz and Chogha Ahovan. Anatolian Studies 64 (2014): 23-31. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,379,16213,NA,NA,NA,203,3,103,653,60,NA,9.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,26,2359,NA,NA,NA,14,2,7,110,4,NA,0.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"TKY025","TKY025","Eurasia","Persian Belt","Turkey","Bitlis","Nemrut Dag","Nemrut Dag II","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.61,42.248,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Nenezi Dag (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Carter, T. and M.S. Shackley. Sourcing Obsidian from Neolithic Çatalhöyük (Turkey) Using Energy Dispersive X-Ray Fluorescence. Archaeometry 49 (2007) No. 3, 437-454. ; Oddone, M., Z. Yegingil, G. Bigazzi, T. Ercan, and Özdogan. Chemical Characterizations of Anatolian Obsidians by Instrumental and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry 224, 1-2 (1997) 27-38. ; Gratuze, B. Obsidian Characterization by Laser Ablation ICP-MS and its Application to Prehistoric Trade in the Mediterranean and the Near East: Sources and Distribution of Obsidian within Aegean and Anatolia. Journal of Archaeological Science (1999) 26, 891-881. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Khazaee, M., M. D. Glascock, P. Masjedi, F. Khademi Nadoshan, R. Soleimani Farsani, M. Delfan, A. Mansori, B. Sodaie, and A. Dolatyari. Sourcing the Obsidian of Prehistoric Tools Found in Western Iran to Southeast Turkey: A Case Study for the Sites of Eastern Chia Sabz and Chogha Ahovan. Anatolian Studies 64 (2014): 23-31. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32548.5,NA,35986.5,NA,1258.36842105263,513.892857142857,10340.8260869565,NA,46.7869565217391,17.8888888888889,172.28,106.220833333333,18.9090909090909,135.416666666667,19.1117391304348,1.234,7.321,545.875,42.4714285714286,65.6857142857143,NA,NA,NA,NA,0.499833333333333,NA,NA,NA,NA,20,29.6083333333333,7.77714285714286,1080.88652503743,NA,1453.04882580046,NA,182.906217674458,39.5411942991733,950.637804187566,NA,7.57793032600435,3.19722101554181,8.89535735764258,6.17136252448066,3.76502836596104,7.52317084056687,2.03847075590432,0.005,0.72636056916196,57.4074612817678,2.10542038970972,3.66590257232084,NA,NA,NA,NA,0.0393985072449746,NA,NA,NA,NA,3.18550343316712,3.84712955569638,0.488662312948334,35
"TKY026","TKY026","Eurasia","Persian Belt","Turkey","Bitlis","Nemrut Dag","Nemrut Dag III","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.61,42.248,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khazaee, M., M. D. Glascock, P. Masjedi, F. Khademi Nadoshan, R. Soleimani Farsani, M. Delfan, A. Mansori, B. Sodaie, and A. Dolatyari. Sourcing the Obsidian of Prehistoric Tools Found in Western Iran to Southeast Turkey: A Case Study for the Sites of Eastern Chia Sabz and Chogha Ahovan. Anatolian Studies 64 (2014): 23-31. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,686,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7.3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,39,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3
"TKY027","TKY027","Eurasia","Persian Belt","Turkey","Bitlis","Nemrut Dag","Nemrut Dag IV","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.61,42.248,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khazaee, M., M. D. Glascock, P. Masjedi, F. Khademi Nadoshan, R. Soleimani Farsani, M. Delfan, A. Mansori, B. Sodaie, and A. Dolatyari. Sourcing the Obsidian of Prehistoric Tools Found in Western Iran to Southeast Turkey: A Case Study for the Sites of Eastern Chia Sabz and Chogha Ahovan. Anatolian Studies 64 (2014): 23-31. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,774,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9.2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"TKY028","TKY028","Eurasia","Persian Belt","Turkey","Bitlis","Nemrut Dag","Nemrut Dag V","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.61,42.248,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khazaee, M., M. D. Glascock, P. Masjedi, F. Khademi Nadoshan, R. Soleimani Farsani, M. Delfan, A. Mansori, B. Sodaie, and A. Dolatyari. Sourcing the Obsidian of Prehistoric Tools Found in Western Iran to Southeast Turkey: A Case Study for the Sites of Eastern Chia Sabz and Chogha Ahovan. Anatolian Studies 64 (2014): 23-31. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,727,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,61.7776856847625,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.603588740733681,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"TKY032","TKY032","Eurasia","Persian Belt","Turkey","Kars","Sarikamis","Sarikamis I","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",40.177,42.792,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Sarikamis South I (IAOS World Source Catalog). (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,551,597,9522,NA,60.2,NA,134,20.6,30.3,130.9,19.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10.3717246962457,50.7307817796468,1464.6772964424,NA,8.89748160055994,NA,12.9545807813373,4.40158342247439,3.74386627553045,14.9556706248127,2.70623775181922,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"TKY033","TKY033","Eurasia","Persian Belt","Turkey","Kars","Sarikamis","Sarikamis II","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",40.177,42.792,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Sarikamis South II (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,518.6,308.6,5398,NA,31.68,NA,119.4,16.78,15.92,72.56,12.02,NA,NA,381.25,22.5,40.25,NA,NA,NA,NA,0.3425,NA,NA,NA,NA,NA,14.25,6.1,NA,NA,NA,NA,32.9504678773054,18.149380154705,830.322206069743,NA,3.77747711221833,NA,3.4253953543107,1.44083309234623,1.27645341996225,8.69409761466556,0.650128192487195,NA,NA,50.7370673176919,3.51188458428425,4.99165971062398,NA,NA,NA,NA,0.0170782512765993,NA,NA,NA,NA,NA,1.5,0.336650164612069,10
"TKY041","TKY041","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 4a","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.297,34.544,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,324,NA,NA,NA,NA,NA,192,6.7,21,69,27,NA,NA,77,22,42,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19,8.4,NA,NA,NA,NA,12,NA,NA,NA,NA,NA,6,0.5,2,6,1,NA,NA,4,2,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2,0.6,17
"TKY042","TKY042","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 4b","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.307,34.548,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,342,NA,NA,NA,NA,NA,187,7.6,20,68,26,NA,NA,98,22,41,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19,7.9,NA,NA,NA,NA,14,NA,NA,NA,NA,NA,7,1.6238851461556,2,7,1.2,NA,NA,9,2,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3,0.937171209421318,18
"TKY043","TKY043","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 5","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.283,34.57,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,351,NA,NA,NA,NA,NA,188,9,20,70,25,NA,NA,126,22,42,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20,8.3,NA,NA,NA,NA,13,NA,NA,NA,NA,NA,6,0.7,2,5,0.7,NA,NA,8,2,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2,0.3,51
"TKY044","TKY044","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 6","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.252,34.511,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,306,NA,NA,NA,NA,NA,193,8.6,21,66,25,NA,NA,90,21,41,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,17,8.6,NA,NA,NA,NA,21,NA,NA,NA,NA,NA,7,0.8,2,6,1.1,NA,NA,9,2,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2,0.6,5
"TKY045","TKY045","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","Acigöl (the wall of the maar)","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Acigöl (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33800,NA,37200,NA,350,535,7050,NA,44.75,NA,241.5,3.835,NA,86.9,33.2,0.574,13.85,9.6,17.65,30.2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,35.05,12.65,619.974746830583,NA,500,NA,17.0710678118655,30.6066017177982,235.355339059327,NA,0.663908729652599,NA,3.47487373415292,0.0563908729652602,NA,0.765685424949241,0.437132034355965,0.0220355339059327,0.301776695296637,0.270710678118655,0.210355339059327,1.79705627484771,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.967462120245875,0.306776695296637,2
"TKY046","TKY046","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","Acigöl-Bogazköy General","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Acigöl (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33500,NA,36800,NA,460,506.666666666667,10100,NA,35.6666666666667,NA,184.666666666667,81.5333333333333,NA,153.333333333333,20.2666666666667,0.525333333333333,8.09666666666667,399.333333333333,37.1666666666667,46.6333333333333,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28.3,8.65333333333333,216.666666666667,NA,300,NA,16.6666666666667,16.2200846792815,747.743619705559,NA,0.541987021599052,NA,3.58795820974478,0.967736009766474,NA,2.92497240587846,0.563578360739103,0.0298102535890733,0.449490617998676,2.12200846792815,1.33988794990677,2.10963611526676,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.65,0.312799511487263,3
"TKY047","TKY047","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","Acigöl-Bogazköy (the wall of the caldera)","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Acigöl (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33400,NA,36700,NA,470,500,8700,NA,35.7,NA,156,78.9,NA,151,22.3,0.567,7.31,401,26.9,43.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27.6,8.01,400,NA,400,NA,30,20,300,NA,0.4,NA,3,0.9,NA,4,0.5,0.04,0.05,2,0.5,0.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.6,0.04,1
"TKY048","TKY048","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","Acigöl-Güney Dagi","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Acigöl (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33500,NA,37750,NA,360,580,7900,NA,43.84,NA,246,3.56,NA,87.55,33.435,0.567,14.65,9.2,18.8,31.3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36.7,12.65,220.710678118655,NA,547.487373415292,NA,19.5710678118655,24.5710678118655,1468.50288425444,NA,0.526616882454316,NA,9.57106781186548,0.10278174593052,NA,0.967462120245873,0.973558620695906,0.0316555915910215,0.867462120245875,0.245710678118655,0.761396103067893,2.69129509039023,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.77058441227157,0.757462120245875,2
"TKY049","TKY049","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","Acigöl-Kocadag","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Acigöl (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32550,NA,37600,NA,420,525,8700,NA,41.75,NA,232,3.95,NA,86.1,32.2,0.516,7.1,21.2,25.45,38.75,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,22.35,9.1,281.066017177982,NA,291.42135623731,NA,131.213203435596,42.2487373415292,1327.08152801713,NA,0.488908729652599,NA,7.40685424949238,0.373553390593274,NA,0.66997474683058,0.297132034355965,0.0111997474683058,1.28529220613579,8.17388527117068,3.62517856687341,4.07444263558534,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.17530483272049,2.37024169979695,2
"TKY050","TKY050","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","Acigöl-Taskesiktepe","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Acigöl (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32770,NA,36500,NA,190,450,10800,NA,37.7,NA,221,4.98,NA,92.3,29.4,0.523,5.35,6.1,31.8,43.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.7,5.3,300,NA,300,NA,20,10,500,NA,0.2,NA,5,0.03,NA,0.5,0.4,0.04,0.02,0.9,0.5,0.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.2,0.05,1
"TKY051","TKY051","Eurasia","Persian Belt","Turkey","Bingol","Bingöl Dag","Bingöl Dag Group General","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.954,40.881,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., Z. Yegingil, G. Bigazzi, T. Ercan, and Özdogan. Chemical Characterizations of Anatolian Obsidians by Instrumental and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry 224, 1-2 (1997) 27-38. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42960,NA,37840,NA,1556.6,506,19240,NA,126.2,NA,155.76,1.326,NA,241.8,66.86,0.812,6.8204,502,36.5,63.82,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25.1,8.966,455.277606521376,NA,489.434968935316,NA,29.8694122363317,31.2479506819769,3603.19295395395,NA,3.35192024052026,NA,20.6936239911822,0.0639225476325092,NA,41.4674928072664,0.882317591976736,0.298711813506974,0.293746087415722,33.8655147594632,4.56644285437724,11.1248606623945,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4.64451114648293,0.51178325104497,5
"TKY052","TKY052","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","East Acigöl 1","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is Ante Caldera (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gratuze, B. Obsidian Characterization by Laser Ablation ICP-MS and its Application to Prehistoric Trade in the Mediterranean and the Near East: Sources and Distribution of Obsidian within Aegean and Anatolia. Journal of Archaeological Science (1999) 26, 891-881. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33,NA,163,74,22,140,19,NA,NA,363,30,52,NA,NA,NA,NA,0.36,NA,NA,NA,NA,18,27,8.4,NA,NA,NA,NA,NA,NA,NA,NA,6,NA,17,18,1,5,1,NA,NA,45,3,5,NA,NA,NA,NA,0.0494375841473839,NA,NA,NA,NA,2.86695308985041,5,1.8,6
"TKY053","TKY053","Eurasia","Persian Belt","Turkey","Nevsehir","Acigöl","East Acigöl 2","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is Ante Caldera (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gratuze, B. Obsidian Characterization by Laser Ablation ICP-MS and its Application to Prehistoric Trade in the Mediterranean and the Near East: Sources and Distribution of Obsidian within Aegean and Anatolia. Journal of Archaeological Science (1999) 26, 891-881. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25,NA,147,54,19,92,15,NA,NA,260,22,39,NA,NA,NA,NA,0.21,NA,NA,NA,NA,19,21,6.7,NA,NA,NA,NA,NA,NA,NA,NA,6,NA,28,11,3,16,3,NA,NA,51,5,9,NA,NA,NA,NA,0.07,NA,NA,NA,NA,2,7,2.4,11
"TKY054","TKY054","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","East Göllüdag","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.24,34.543,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Carter, T. and M.S. Shackley. Sourcing Obsidian from Neolithic Çatalhöyük (Turkey) Using Energy Dispersive X-Ray Fluorescence. Archaeometry 49 (2007) No. 3, 437-454. ; Hancock, R. G. V. and Tristan Carter. How Reliable are our Published Archaeometric Analyses, Effects of Analytical Techniques Through Time on the Elemental Analysis of Obsidians. Journal of Archaeological Science 37 (2010) 243-250. ; Le Bourdonnec F.-X., S. Delerue, S. Dubernet, Ph. Moretto, Th. Calligro, J.-C. Dran, and G. Poupeau. PIXE Characterization of Western Mediterranean and Anatolian Obsidians and Neolithic Provenance Studies. Nuclear Instruments and Methods in Physics Research B 240 (2005): 595-599. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29594.8918918919,NA,35282.7387387387,NA,461.264705882353,473.970588235294,5948.64705882353,NA,26.4166666666667,18.3076923076923,185.697080745342,13.5186335403727,21.87275,76.1436645962733,24.16525,NA,NA,145.822074074074,22.1243703703704,42.3694074074074,NA,NA,NA,NA,0.146,NA,NA,NA,NA,21.955037037037,21.9578125,8.06614814814815,1414.94546903384,NA,1740.52747397103,NA,206.242098702746,45.0925887895959,1065.16993336367,NA,7.13160143944688,4.00768492543244,9.95129036118021,3.39595678142619,1.6072689677963,4.33210296960009,1.98374623571688,NA,NA,22.456000478547,1.33310579745434,2.69315499145968,NA,NA,NA,NA,0.0157998908812521,NA,NA,NA,NA,0.998579623805055,3.70949387937573,0.560936392354667,161
"TKY055","TKY055","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag Group General","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.24,34.543,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., Z. Yegingil, G. Bigazzi, T. Ercan, and Özdogan. Chemical Characterizations of Anatolian Obsidians by Instrumental and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry 224, 1-2 (1997) 27-38. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30900,NA,38400,NA,410,490,8600,NA,25.9046666666667,NA,162.533333333333,51.1713333333333,18.4285714285714,92.92,18.4066666666667,0.98,7,439.466666666667,32.9133333333333,54.5266666666667,NA,NA,NA,NA,0.307142857142857,NA,NA,NA,NA,19.1428571428571,26.7533333333333,7.26,400,NA,300,NA,40,50,400,NA,6.51612118485313,NA,11.8619071008638,13.0629144083842,1.71069624773613,19.9736638330782,1.53670150132459,0.002,0.02,59.6207374905751,5.4077404590893,8.22869067448294,NA,NA,NA,NA,0.0850681817353607,NA,NA,NA,NA,2.98205266725208,5.1068725619956,0.936271745650596,15
"TKY056","TKY056","Eurasia","Persian Belt","Turkey","Nigde","Kömürcü","Kömürcü Group General","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.283,34.57,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Kömürcü, Göllü Dagi-Kömürcü (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Oddone, M., Z. Yegingil, G. Bigazzi, T. Ercan, and Özdogan. Chemical Characterizations of Anatolian Obsidians by Instrumental and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry 224, 1-2 (1997) 27-38. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31600,NA,38025,NA,382.5,487.5,6750,NA,21.9,NA,179.625,18.7675,NA,77.95,19.7,1.1165,6.405,169.75,30.65,43.75,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24.7,8.11,379.047594742265,NA,162.5,NA,29.9303940559741,23.6410973973775,489.991721763537,NA,0.4139087296526,NA,1.94939327352725,1.6151795008071,NA,0.885982755730146,0.277487373415291,0.0163314754519511,0.51143921292465,4.01245860881769,1.52885822331377,0.688908729652599,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.316421356237309,0.905746391493337,4
"TKY057","TKY057","Eurasia","Persian Belt","Turkey","Bitlis","Nemrut Dag","Nemrut Dag Group General","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.61,42.248,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Lake Van, Nemrut Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Boulanger, Matthew T, Richard S. Davis, and Michael D. Glascock. Preliminary Characterization and Regional Comparison of the Dash-i-Nawur Obsidian Source Near Ghazni, Afghanistan. Journal of Archaeological Science 39 (2012) 2320-2328. ; Khazaee, M., M. D. Glascock, P. Masjedi, F. Khademi Nadoshan, R. Soleimani Farsani, M. Delfan, A. Mansori, B. Sodaie, and A. Dolatyari. Sourcing the Obsidian of Prehistoric Tools Found in Western Iran to Southeast Turkey: A Case Study for the Sites of Eastern Chia Sabz and Chogha Ahovan. Anatolian Studies 64 (2014): 23-31. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,41864,NA,37488,NA,402,758.8,20593.5909090909,NA,192.06,NA,234.886363636364,1.4375,136,1225.75,74.5416666666667,1.6042,12.83,77.6588,104.968,212.024,NA,NA,NA,NA,0.81,NA,NA,NA,NA,NA,29.6,10.5724,4203.7410618295,NA,1901.60241619406,NA,315.969053814876,353.851160721123,16097.1975506784,NA,50.8296571678412,NA,19.8052183507329,1.30991076320621,12,200.845222353542,3.98804527731852,0.12867858369323,0.622624601910666,200.365354738196,22.6872324507001,26.4077706626977,NA,NA,NA,NA,0.111234564331614,NA,NA,NA,NA,NA,3.43026368608932,1.08678832914613,44
"TKY058","TKY058","Eurasia","Persian Belt","Turkey","Bitlis","Süphaun Dag","Süphaun Dag Group General","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",38.931,42.829,"","","Lake Van Volcanic Area","","Obsidian","","","""Literature suggests alternate names for this source include: Mount Süphan (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Boulanger, Matthew T, Richard S. Davis, and Michael D. Glascock. Preliminary Characterization and Regional Comparison of the Dash-i-Nawur Obsidian Source Near Ghazni, Afghanistan. Journal of Archaeological Science 39 (2012) 2320-2328. ; Oddone, M., Z. Yegingil, G. Bigazzi, T. Ercan, and Özdogan. Chemical Characterizations of Anatolian Obsidians by Instrumental and Epithermal Neutron Activation Analysis. Journal of Radioanalytical and Nuclear Chemistry 224, 1-2 (1997) 27-38. ; Innocenti, F., R. Mazzuoli, G. Pasquare, F. Radicati di Brozolo, and L. Villari. Evolution of the Volcanism in the Area of Interaction Between the Arabian, Anatolian, and Iranian Plates (Lake Van, Eastern Turkey). Journal of Volcanology and Geothermal Research 1 (1976) 103-112.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19273.5294117647,NA,21761.7647058824,NA,2780,374.411764705882,8392.94117647059,NA,51.6882352941176,NA,105.470588235294,21.8352941176471,NA,239.976470588235,34.65,0.847,6.065,126.176470588235,26.8941176470588,54.1470588235294,NA,NA,NA,NA,0.3,NA,NA,NA,NA,NA,14.5158823529412,5.24941176470588,11244.9105224315,NA,7555.70915724684,NA,1657.98773235279,177.119357607729,5148.48879041917,NA,41.647031528966,NA,75.9405343009029,21.6017747903001,NA,198.18958479407,0.235355339059328,0.0519974746830583,0.573007755419574,198.322021112979,16.711307477587,35.3715236318111,NA,NA,NA,NA,0.3,NA,NA,NA,NA,NA,10.89847540468,2.31823789555263,17
"TKY060","TKY060","Eurasia","Persian Belt","Turkey","Kars","Sarikamis","Sarikamis Group general","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",40.177,42.792,"","Aragats","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32814.2857142857,NA,38671.4285714286,NA,832.857142857143,562.857142857143,7175.71428571429,NA,40.7557142857143,NA,145.857142857143,23.4428571428571,NA,138.428571428571,14.1414285714286,0.984571428571429,4.67428571428571,678.714285714286,33.9857142857143,48.6285714285714,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,17.9714285714286,6.33285714285714,2135.20524829105,NA,759.31397459497,NA,34.394496126416,456.785569458903,733.829403931944,NA,7.77268839550372,NA,4.51977608756802,0.367551125713401,NA,4.3630840071478,0.595884347342549,1.05141085145685,0.238336882887962,35.6260899714615,1.47903748729209,2.61964219231987,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.897783529124006,0.312124383648057,7
"TKY061","TKY061","Eurasia","Persian Belt","Turkey","Bitlis","Nemrut Dag","Nemrut Dag VI","","23-0",11.5,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",38.61,42.248,"","Lake Van Volcanic Area","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khazaee, M., M. D. Glascock, P. Masjedi, F. Khademi Nadoshan, R. Soleimani Farsani, M. Delfan, A. Mansori, B. Sodaie, and A. Dolatyari. Sourcing the Obsidian of Prehistoric Tools Found in Western Iran to Southeast Turkey: A Case Study for the Sites of Eastern Chia Sabz and Chogha Ahovan. Anatolian Studies 64 (2014): 23-31. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578. ; Innocenti, F., R. Mazzuoli, G. Pasquare, F. Radicati di Brozolo, and L. Villari. Evolution of the Volcanism in the Area of Interaction Between the Arabian, Anatolian, and Iranian Plates (Lake Van, Eastern Turkey). Journal of Volcanology and Geothermal Research 1 (1976) 103-112. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1379,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,26,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"TKY062","TKY062","Eurasia","Persian Belt","Turkey","Nigde","Göllüdag","Göllüdag 3","","0.9-0.86",0.88,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",38.257,34.551,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Binder, Didier, Bernard Gratuze, Damase Mouralis, and Nur Balkan-Atli. New Investigations of the Göllüdağ Obsidian Lava Flows System: A Multi-Disciplinary Approach. Journal of Archaeological Science 38 (2011) 3174-3184. ; Topra, Vedat and M. C. Göncüoḡlu. Tectonic Control of the Development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28 (1993) 357-369.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,331,NA,NA,NA,NA,NA,181,13,17,74,22,NA,NA,194,18,39,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,18,8,NA,NA,NA,NA,6.230564200467,NA,NA,NA,NA,NA,17.4983516524034,2.77769827631879,2.10051903247583,8.45469538759465,3.06892940927953,NA,NA,21.3936435145873,1.54776049634055,5.21779134672288,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.99964773340095,0.949034136122854,1
"TKY065","TKY065","Eurasia","Persian Belt","Turkey","Kars","Sarikamis","North Sarikamis","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",40.177,42.792,"","Aragats","","","Obsidian","","","""Literature suggests alternate names for this source include: Kizil Kilisa (IAOS World Source Catalog). (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Chataigner, C. and B. Gratuze. New Data on the Exploitation of Obsidian In the Southern Caucasus (Armenia, Georgia) and Eastern Turkey, Part 2: Obsidian Procurement from the Upper Paleolithic to the Late Bronze Age. Archaeometry 56, 1 (2014) 48-69. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,456.777777777778,599.111111111111,NA,NA,71,NA,129.555555555556,2.03333333333333,36.3333333333333,167.222222222222,27.2222222222222,NA,NA,29.2222222222222,31.2222222222222,62.3333333333333,NA,NA,NA,NA,0.232222222222222,NA,NA,NA,NA,NA,17.1111111111111,6.62222222222222,NA,NA,NA,NA,32.9877923548158,19.0685896466181,NA,NA,4.21307488658818,NA,3.35824027993498,0.7,1.3228756555323,19.4214943926683,0.833333333333333,NA,NA,6.20035841257942,3.30823887354653,4.55521678957215,NA,NA,NA,NA,0.0486769395550341,NA,NA,NA,NA,NA,0.927960727138337,0.268224615657185,9
"YEM002","YEM002","Eurasia","African Rift","Yemen","Dhamar","Hayd al Halal","Hayd al Halal 1","","30",30,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",14.563,44.708,"","Dhamar","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khalidi, Lamya, Clive Oppenheimer, Bernard Gratuze, Sophie Boucetta, Ali Sanabani, and Ahmed al-Mosabi. Obsidian Sources in Highland Yemen and their Relevance to Archaeological Research in the Red Sea Region. Journal of Archaeological Science 37 (2010) 2332-2345.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,599,454,11281,NA,NA,NA,164,4.3,55,274,NA,NA,NA,32,52,119,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,15,4,NA,NA,NA,NA,55,40,2984,NA,NA,NA,23,1,11,42,NA,NA,NA,5,9,18,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3,0.7,18
"YEM003","YEM003","Eurasia","African Rift","Yemen","Dhamar","Hayd al Halal","Hayd al Halal 2","","30",30,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",14.563,44.708,"","Dhamar","","High","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khalidi, Lamya, Clive Oppenheimer, Bernard Gratuze, Sophie Boucetta, Ali Sanabani, and Ahmed al-Mosabi. Obsidian Sources in Highland Yemen and their Relevance to Archaeological Research in the Red Sea Region. Journal of Archaeological Science 37 (2010) 2332-2345.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1015,486,11117,NA,NA,NA,178,33,37,264,NA,NA,NA,306,54,116,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,15,4.6,NA,NA,NA,NA,56,38,2309,NA,NA,NA,13,8,8,44,NA,NA,NA,53,9,12,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2,0.9,4
"YEM008","YEM008","Eurasia","African Rift","Yemen","Dhamar","Isbil","Isbil 1","","0",0,"Pyroclastic Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",14.538,44.521,"Location is Questionable","Dhamar","","High","Obsidian","","","""Literature suggests alternate names for this source include: Jebel Isbil (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khalidi, Lamya, Clive Oppenheimer, Bernard Gratuze, Sophie Boucetta, Ali Sanabani, and Ahmed al-Mosabi. Obsidian Sources in Highland Yemen and their Relevance to Archaeological Research in the Red Sea Region. Journal of Archaeological Science 37 (2010) 2332-2345.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1880,1589,46037,NA,NA,NA,245,1.1,169,1770,NA,NA,NA,14,170,319,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32,7,NA,NA,NA,NA,304,133,11586,NA,NA,NA,14,0.3,18,158,NA,NA,NA,2,19,32,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3,0.9,15
"YEM009","YEM009","Eurasia","African Rift","Yemen","Dhamar","Isbil","Isbil 2","","0",0,"Pyroclastic Cone","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",14.538,44.521,"Location is Questionable","Dhamar","","High","Obsidian","","","""Literature suggests alternate names for this source include: Jebel Isbil (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khalidi, Lamya, Clive Oppenheimer, Bernard Gratuze, Sophie Boucetta, Ali Sanabani, and Ahmed al-Mosabi. Obsidian Sources in Highland Yemen and their Relevance to Archaeological Research in the Red Sea Region. Journal of Archaeological Science 37 (2010) 2332-2345.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1418,1071,37617,NA,NA,NA,271,0.2,152,1852,NA,NA,NA,1.8,173,336,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,35,8.2,NA,NA,NA,NA,63,118,9253,NA,NA,NA,20,0.0427338196356737,6,289,NA,NA,NA,0.6,22,39,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2,1,3
"YEM010","YEM010","Eurasia","African Rift","Yemen","Dhamar","Yafa' Ridge","Yafa' Ridge 1","","33.9-23",28.45,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",14.648,44.364,"","Dhamar","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khalidi, Lamya, Clive Oppenheimer, Bernard Gratuze, Sophie Boucetta, Ali Sanabani, and Ahmed al-Mosabi. Obsidian Sources in Highland Yemen and their Relevance to Archaeological Research in the Red Sea Region. Journal of Archaeological Science 37 (2010) 2332-2345.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1036,431,21578,NA,NA,NA,286,0.2,97,1015,NA,NA,NA,1,68,172,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27,7.1,NA,NA,NA,NA,92,42,11093,NA,NA,NA,38,0.1,12,107,NA,NA,NA,0.4,9,19,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3,1.5,31
"YEM011","YEM011","Eurasia","African Rift","Yemen","Dhamar","Yafa' Ridge","Yafa' Ridge 2","","33.9-23",28.45,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",14.648,44.364,"","Dhamar","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khalidi, Lamya, Clive Oppenheimer, Bernard Gratuze, Sophie Boucetta, Ali Sanabani, and Ahmed al-Mosabi. Obsidian Sources in Highland Yemen and their Relevance to Archaeological Research in the Red Sea Region. Journal of Archaeological Science 37 (2010) 2332-2345.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1239,399,34277,NA,NA,NA,172,0.4,66,682,NA,NA,NA,1.8,72,167,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19,3.9,NA,NA,NA,NA,23.3222629739535,33.9054973703167,5272.49986244027,NA,NA,NA,16.6282678685823,0.0854676392713474,8.15495624372969,77.9203007343183,NA,NA,NA,0.198497723331223,6.19104198536219,22.3428501257108,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.11073927414544,0.462654141359891,4
"YEM012","YEM012","Eurasia","African Rift","Yemen","Dhamar","Yafa' Ridge","Yafa' Ridge 3","","33.9-23",28.45,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",14.648,44.364,"","Dhamar","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Khalidi, Lamya, Clive Oppenheimer, Bernard Gratuze, Sophie Boucetta, Ali Sanabani, and Ahmed al-Mosabi. Obsidian Sources in Highland Yemen and their Relevance to Archaeological Research in the Red Sea Region. Journal of Archaeological Science 37 (2010) 2332-2345.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1493,507,34041,NA,NA,NA,124,2.2,39,373,NA,NA,NA,27,77,179,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12,2.7,NA,NA,NA,NA,28.103421000898,43.0829252299513,5236.19826173029,NA,NA,NA,11.9878210215361,0.470072015992411,4.81883778038573,42.616234859092,NA,NA,NA,2.97746584996834,6.6209754565679,23.9483243862409,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.33309848893396,0.320299020941463,1
"CAN033","CAN033","North America","Cascadia","Canada","Yukon","Hoodo Mountain","Hoodo Mountain A","","",NA,"","Active","Convergent","Continental","Active Continental Margin",60.71,-138.213,"","","Wrangell Volcanic Belt","","","","","","""James, Malcom A., Jeff Bailey, and John M. D'Auria. A Volcanic Glass Library for the Pacific Northwest: Problems and Prospects. Canadian Journal of Archaeology 20 (1996) 93-122.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,11.446,0.019,NA,0.773,0.274,0.321,0.178,0.094,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.841,0.008,NA,0.056,0.027,0.02,0.094,0.032,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"CAN034","CAN034","North America","Cascadia","Canada","Yukon","Hoodo Mountain","Hoodo Mountain B","","",NA,"","Active","Convergent","Continental","Active Continental Margin",60.71,-138.213,"","","Wrangell Volcanic Belt","","","","","","""James, Malcom A., Jeff Bailey, and John M. D'Auria. A Volcanic Glass Library for the Pacific Northwest: Problems and Prospects. Canadian Journal of Archaeology 20 (1996) 93-122.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12.066,0.022,NA,0.928,0.182,0.394,0.195,0.133,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.679,0.005,NA,0.087,0.04,0.038,0.017,0.02,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"CAN035","CAN035","North America","Cascadia","Canada","British Columbia","Graham Island","Graham Island 1","","",NA,"","Active","Convergent","Continental","Active Continental Margin",53.539,-132.75,"","","Queen Charolette Islands","","Obsidian","","","""Literature suggests alternate names for this source include: Queen Charlotte Islands (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.181,0.015,NA,0.112,0.118,0.128,0.208,0.07,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.115,0.001,NA,0.006,0.002,0.01,0.011,0.005,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"CAN036","CAN036","North America","Cascadia","Canada","British Columbia","Graham Island","Graham Island 2","","",NA,"","Active","Convergent","Continental","Active Continental Margin",53.539,-132.75,"","","Queen Charolette Islands","","Obsidian","","","""Literature suggests alternate names for this source include: Queen Charlotte Islands (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.917,0.014,NA,0.09,0.104,0.105,0.205,0.066,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.122,0.001,NA,0.003,0.005,0.004,0.014,0.012,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"GUA010","GUA010","North America","Mesoamerica","Guatemala","Chimaltenango","San Martín Jilotepeque","San Martín Jilotepeque Group General","","0",0,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",14.844,-90.736,"","Representative Pixcayá Group","Central Highlands","Medium","Obsidian","""San Martín obsidian is dark grey with possible irregular black banding, but frequently has particulates that can give it an overall red-brown hue. The quality of this glass is highly variable. Inclusions are common from dust to sand grain size and can occur in cloud-like formations (Doering 2002). Deposits are typically difficult to reach and are exposed on the banks of the Pixcayá River (Stross et al 1981).""","""Use of this source peaked during the Middle Formative period, when it became the dominant material throughout the Mayan Lowlands and the Chiapas Highlands (Doering 2002).""","""Literature suggests alternate names for this source include: Aldea, Chatalun, Chimaltenango, Choatalum, Inyaalchay, Las Burras, Pachay, Pixcayá, Río Pixcayá, Sauces Type C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stross, Fred H., Payson Sheets, Frank Asaro, and Helen V. Michel. Precise Characterization of Guatemalan Obsidian Sources, and Source Determination of Artifacts from Quirigua. American Antiquity 48, 2 (1981) 323-346. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29400,NA,35878.3636363636,NA,770.666666666667,487.818181818182,6639.27272727273,NA,26.6666666666667,14,116.2,194.764705882353,12.3333333333333,113.352941176471,6.66666666666667,NA,NA,1105,26.3,NA,NA,NA,NA,NA,0.543,NA,NA,NA,NA,NA,9.24,2.81,500,NA,2211.16718686767,NA,254.433357351848,54.4112560275715,295.79167369688,NA,3.05505046330389,1.47685411511676,7.07966253614681,12.5096442274847,1.52752523165195,4.97610893576903,0.577350269189626,NA,NA,32,0.5,NA,NA,NA,NA,NA,0.1,NA,NA,NA,NA,NA,0.12,0.05,25
"GUA017","GUA017","North America","Mesoamerica","Guatemala","Chimaltenango","San Martín Jilotepeque","San Martín Jilotepeque 1","","0",0,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",14.7409,-90.7848,"","Representative Pixcayá Group","Central Highlands","Medium","Obsidian","""San Martín obsidian is dark grey with possible irregular black banding, but frequently has particulates that can give it an overall red-brown hue. The quality of this glass is highly variable. Inclusions are common from dust to sand grain size and can occur in cloud-like formations (Doering 2002). Deposits are typically difficult to reach and are exposed on the banks of the Pixcayá River (Stross et al 1981). San Martín Jilotepeque 1 deposits can be found in at least five locations across the complex (Braswell and Glascock 1998).""","""Use of this source peaked during the Middle Formative period, when it became the dominant material throughout the Mayan Lowlands and the Chiapas Highlands. San Martín Jilotepeque 1 was the most exploited subsource throughout the Formative Period (Doering 2002).""","""Literature suggests alternate names for this source include: Aldea, Choatalun, Chimaltenango, Choatalum, Inyaalchay, Las Burras, Pachay, Pixcayá, Río Pixcayá, Sauces Type C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stross, Fred H., Payson Sheets, Frank Asaro, and Helen V. Michel. Precise Characterization of Guatemalan Obsidian Sources, and Source Determination of Artifacts from Quirigua. American Antiquity 48, 2 (1981) 323-346. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Braswell, Geoffrey E. and Michael D. Glascock. Interpreting Intrasource Variation in the Composition of Obsidian: The Geoarchaeology of San Martín Jilotepeque, Guatemala. Latin American Antiquity 9, 4 (1998) 353-369. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28500,NA,32400,NA,NA,532,6230,0.284,31.4,NA,108,191,NA,117,NA,0.342,3.15,1046,25.4,45.8,16.1,0.331,1.86,2.88,0.526,1.39,0.221,3.16,0.781,NA,8.33,2.86,400,NA,1700,0.02,NA,10,150,0.012,1,NA,2,15,NA,6,NA,0.054,0.04,12,0.5,0.9,0.7,0.008,0.29,0.05,0.009,0.03,0.006,0.05,0.011,NA,0.12,0.19,28
"GUA018","GUA018","North America","Mesoamerica","Guatemala","Chimaltenango","San Martín Jilotepeque","San Martín Jilotepeque 2","","0",0,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",14.7531,-90.7531,"","Representative Pixcayá Group","Central Highlands","Medium","Obsidian","""San Martín obsidian is dark grey with possible irregular black banding, but frequently has particulates that can give it an overall red-brown hue. The quality of this glass is highly variable. Inclusions are common from dust to sand grain size and can occur in cloud-like formations (Doering 2002). Deposits are typically difficult to reach and are exposed on the banks of the Pixcayá River (Stross et al 1981). San Martín Jilotepeque 2 consists of an extensive flow from a rhyolite dome to the southwest of the complex (Braswell and Glascock 1998).""","""Use of this source peaked during the Middle Formative period, when it became the dominant material throughout the Mayan Lowlands and the Chiapas Highlands (Doering 2002).""","""Literature suggests alternate names for this source include: Aldea, Chatalun, Chimaltenango, Choatalum, Inyaalchay, Las Burras, Pachay, Pixcayá, Río Pixcayá, Sauces Type C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stross, Fred H., Payson Sheets, Frank Asaro, and Helen V. Michel. Precise Characterization of Guatemalan Obsidian Sources, and Source Determination of Artifacts from Quirigua. American Antiquity 48, 2 (1981) 323-346. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Braswell, Geoffrey E. and Michael D. Glascock. Interpreting Intrasource Variation in the Composition of Obsidian: The Geoarchaeology of San Martín Jilotepeque, Guatemala. Latin American Antiquity 9, 4 (1998) 353-369. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28800,NA,34100,NA,2235,568.9,5991.6,0.321,29.98,NA,119.3,131.9,19,109.7,13,0.38,3.97,1012,21.6,40.7,14.4,0.37,2.23,2.96,0.487,1.63,0.257,3.05,0.837,NA,10.268,3.17,400,NA,2200,0.03,42.0704259457515,22.031222920257,277.078210486802,0.031,6.79325035256027,NA,2.97487373415292,12.9246212024587,2.34763891864946,16.6317279836453,1.81345828730154,0.063,0.337499619818692,13,0.5,0.6,1.96032326147017,0.014,0.22,0.05,0.007,0.04,0.005,0.38,0.007,NA,6.22511326757043,0.07,10
"GUA019","GUA019","North America","Mesoamerica","Guatemala","Chimaltenango","San Martín Jilotepeque","San Martín Jilotepeque 3","","0",0,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",14.7694,-90.7662,"","Representative Pixcayá Group","Central Highlands","Medium","Obsidian","""San Martín obsidian is dark grey with possible irregular black banding, but frequently has particulates that can give it an overall red-brown hue. The quality of this glass is highly variable. Inclusions are common from dust to sand grain size and can occur in cloud-like formations (Doering 2002). Deposits are typically difficult to reach and are exposed on the banks of the Pixcayá River (Stross et al 1981). San Martín Jilotepeque 3 can be found on the same ridge as San Martín Jilotepeque 2 (towards the southwest of the complex), and is composed of two deposits (Braswell and Glascock 1998).""","""Use of this source peaked during the Middle Formative period, when it became the dominant material throughout the Mayan Lowlands and the Chiapas Highlands (Doering 2002).""","""Literature suggests alternate names for this source include: Aldea, Chatalun, Chimaltenango, Choatalum, Inyaalchay, Las Burras, Pachay, Pixcayá, Río Pixcayá, Sauces Type C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stross, Fred H., Payson Sheets, Frank Asaro, and Helen V. Michel. Precise Characterization of Guatemalan Obsidian Sources, and Source Determination of Artifacts from Quirigua. American Antiquity 48, 2 (1981) 323-346. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Braswell, Geoffrey E. and Michael D. Glascock. Interpreting Intrasource Variation in the Composition of Obsidian: The Geoarchaeology of San Martín Jilotepeque, Guatemala. Latin American Antiquity 9, 4 (1998) 353-369. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30400,NA,32100,NA,NA,602,7630,0.503,31.9,NA,111,185,NA,131,NA,0.367,3.63,1019,24.1,44.5,16.2,0.373,2.14,3.06,0.575,1.63,0.261,3.51,0.774,NA,8.39,2.95,400,NA,2400,0.05,NA,8,320,0.031,0.8,NA,2,7,NA,5,NA,0.072,0.04,20,0.4,0.8,0.5,0.014,0.31,0.04,0.009,0.03,0.005,0.06,0.012,NA,0.13,0.12,8
"GUA020","GUA020","North America","Mesoamerica","Guatemala","Chimaltenango","San Martín Jilotepeque","San Martín Jilotepeque 4","","0",0,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",14.7681,-90.7749,"","Representative Pixcayá Group","Central Highlands","Medium","Obsidian","""San Martín obsidian is dark grey with possible irregular black banding, but frequently has particulates that can give it an overall red-brown hue. The quality of this glass is highly variable. Inclusions are common from dust to sand grain size and can occur in cloud-like formations (Doering 2002). Deposits are typically difficult to reach and are exposed on the banks of the Pixcayá River (Stross et al 1981). San Martín Jilotepeque 4 represents a minor outcrop from a single flow (Braswell and Glascock 1998).""","""Use of this source peaked during the Middle Formative period, when it became the dominant material throughout the Mayan Lowlands and the Chiapas Highlands (Doering 2002).""","""Literature suggests alternate names for this source include: Aldea, Chatalun, Chimaltenango, Choatalum, Inyaalchay, Las Burras, Pachay, Pixcayá, Río Pixcayá, Sauces Type C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stross, Fred H., Payson Sheets, Frank Asaro, and Helen V. Michel. Precise Characterization of Guatemalan Obsidian Sources, and Source Determination of Artifacts from Quirigua. American Antiquity 48, 2 (1981) 323-346. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Braswell, Geoffrey E. and Michael D. Glascock. Interpreting Intrasource Variation in the Composition of Obsidian: The Geoarchaeology of San Martín Jilotepeque, Guatemala. Latin American Antiquity 9, 4 (1998) 353-369. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28800,NA,31600,NA,NA,523,6200,0.495,27,NA,116,175,NA,100,NA,0.456,4.11,970,19.4,35.8,12.9,0.317,1.93,2.52,0.441,1.22,0.204,2.68,0.812,NA,8.2,2.94,200,NA,1200,0.03,NA,4,100,0.023,0.3,NA,1,10,NA,6,NA,0.086,0.04,11,0.3,0.5,0.3,0.004,0.11,0.02,0.005,0.05,0.004,0.03,0.006,NA,0.09,0.11,4
"GUA021","GUA021","North America","Mesoamerica","Guatemala","Chimaltenango","San Martín Jilotepeque","San Martín Jilotepeque 5","","0",0,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",14.7735,-90.7287,"","Representative Pixcayá Group","Central Highlands","Medium","Obsidian","""San Martín obsidian is dark grey with possible irregular black banding, but frequently has particulates that can give it an overall red-brown hue. The quality of this glass is highly variable. Inclusions are common from dust to sand grain size and can occur in cloud-like formations (Doering 2002). Deposits are typically difficult to reach and are exposed on the banks of the Pixcayá River (Stross et al 1981). San Martín Jilotepeque 5 origintates from a small rhyolite dome to the southeast of the complex (Braswell and Glascock 1998).""","""Use of this source peaked during the Middle Formative period, when it became the dominant material throughout the Mayan Lowlands and the Chiapas Highlands (Doering 2002).""","""Literature suggests alternate names for this source include: Aldea, Chatalun, Chimaltenango, Choatalum, Inyaalchay, Las Burras, Pachay, Pixcayá, Río Pixcayá, Sauces Type C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stross, Fred H., Payson Sheets, Frank Asaro, and Helen V. Michel. Precise Characterization of Guatemalan Obsidian Sources, and Source Determination of Artifacts from Quirigua. American Antiquity 48, 2 (1981) 323-346. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Braswell, Geoffrey E. and Michael D. Glascock. Interpreting Intrasource Variation in the Composition of Obsidian: The Geoarchaeology of San Martín Jilotepeque, Guatemala. Latin American Antiquity 9, 4 (1998) 353-369. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31800,NA,31600,NA,NA,637,8410,0.451,39.9,NA,100,247,NA,166,NA,0.241,2.18,1024,25.8,48.2,18.3,0.392,2.26,3.26,0.666,1.63,0.26,4.49,0.695,NA,6.51,2.35,200,NA,2400,0.02,NA,6,90,0.115964958205221,0.7,NA,1,11,NA,4,NA,0.0180494505730068,0.03,8,0.2,0.6,0.7,0.01,0.42,0.311799913409713,0.008,0.159206303207414,0.007,0.05,0.01,NA,0.07,0.11,10
"GUA022","GUA022","North America","Mesoamerica","Guatemala","Chimaltenango","San Martín Jilotepeque","San Martín Jilotepeque 6","","0",0,"Stratovolcano","Active","Convergent","Continental","Active Continental Margin",14.7458,-90.7448,"","Representative Pixcayá Group","Central Highlands","Medium","Obsidian","""San Martín obsidian is dark grey with possible irregular black banding, but frequently has particulates that can give it an overall red-brown hue. The quality of this glass is highly variable. Inclusions are common from dust to sand grain size and can occur in cloud-like formations (Doering 2002). Deposits are typically difficult to reach and are exposed on the banks of the Pixcayá River (Stross et al 1981). The San Martín Jilotepeque 6 deposit has likely eroded out from its original location (Braswell and Glascock 1998).""","""Use of this source peaked during the Middle Formative period, when it became the dominant material throughout the Mayan Lowlands and the Chiapas Highlands (Doering 2002).""","""Literature suggests alternate names for this source include: Aldea, Chatalun, Chimaltenango, Choatalum, Inyaalchay, Las Burras, Pachay, Pixcayá, Río Pixcayá, Sauces Type C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stross, Fred H., Payson Sheets, Frank Asaro, and Helen V. Michel. Precise Characterization of Guatemalan Obsidian Sources, and Source Determination of Artifacts from Quirigua. American Antiquity 48, 2 (1981) 323-346. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Braswell, Geoffrey E. and Michael D. Glascock. Interpreting Intrasource Variation in the Composition of Obsidian: The Geoarchaeology of San Martín Jilotepeque, Guatemala. Latin American Antiquity 9, 4 (1998) 353-369. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27200,NA,34900,NA,NA,446,7670,0.922,28.2,NA,112,185,NA,116,NA,0.394,4.28,996,25.4,45.4,15.3,0.335,1.84,2.89,0.488,1.32,0.213,3.1,0.899,NA,9.38,3.27,200,NA,1600,0.02,NA,5,40,0.01,1,NA,1,9,NA,7,NA,0.05,0.04,12,4.7,7.6,2.3,0.019,0.186663177113867,0.025,0.022,0.03,0.006,0.03,0.013,NA,0.84,0.387917703140216,10
"MEX015","MEX015","North America","Northern Mexico","Mexico","Chihuahua","Sierra Fresnal","Sierra Fresnal Group General","","",NA,"","Active","Convergent","Continental","Active Continental Margin",30.84,-107.768,"","","","","Obsidian","""Sierra Fresnal is located in northern Chihuahua, and can be found in secondary alluvial deposits for 70 km around (Dolan et al 2016).""","","""Literature suggests alternate names for this source includes Lago Fredrico, Laguna Azteca, Ojo Fredrico (Dolan et al 2017, Shackley 2002).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Source Provenance of Obsidian Artifacts from the Casas Grande Outlier Sites 204, 242, and 315, Northern Chihuahua. Archaeological Research Facility, UC Berkeley (2014). ; Dolan, Sean G., Michael E. Whalen, Paul E. Minnis, and Steen M. Shackley. Obsidian in the Casas Grandes World: Procurement, Exchange, and Interaction in Chihuahua, Mexico, CE 1200-1450. Journal of Archaeological Science 11 (2017) 555-567. ; Shackley, Steven M. Source Provenance of Archaeological Obsidian from Mimbres Mogollon Sites in the Cader Mountains, Southwest New Mexico. Archaeological Research Facility, UC Berkeley (2002).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,879.333333333333,263.5,1324,NA,NA,NA,299.833333333333,38.8333333333333,65.1666666666667,153.166666666667,20,NA,NA,132,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33.3333333333333,44,NA,NA,NA,NA,NA,173.233561028649,13.9247980236699,25.9656409092751,NA,NA,NA,8.68139773692386,1.32916013582513,2.40138848724372,3.18852107828483,2.0976176963403,NA,NA,14.5564997109563,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.94392028877595,5.13809303146605,NA,6
"MEX026","MEX026","North America","Trans-Mexican Volcanic Belt","Mexico","Guanajuato","Penjamo","Penjamo-1","","10",10,"","Active","Convergent","Continental","Active Continental Margin",20.423,-101.75,"","Michoacán-Guanajuato Volcanic Field","Central TMVB","","Obsidian","""Obsidian from Penjamo can be found in a clear grey flow band streching over 8km, immediatly due west of its town namesake in Guanjuato, Mexico. The best exposures can be found near the La Golondrina dam shoreline, where there is copious amounts of tool working debris. There are also vast quantities of obsidian in the 'flows embedded in volcanic ash in some abandoned modern quarries on Mexico Highway 110 on the southern edge of Churipitzeo' (Cobean 2002).""","","""Literature suggests alternate names for this source include: Sierra de Penjamo (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Cobean, R. H. (2002). A World of Obsidian: The Mining and Trade of a Volcanic Glass in Ancient Mexico. Serie Arqueologia de Mexico. Mexico City: Intituto Nacional de Anthropologia e Historia/University of Pittsburgh.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34344.4,NA,37309.775,NA,NA,399.634,16154.033,0.018,129.913,NA,149.62,NA,NA,588.097,NA,0.349,5.099,80.392,56.007,120.353,56.547,1.96,13.536,13.53,0.932,7.965,1.16,16.222,1.74,NA,14.395,4.729,712.133,NA,1697.12,0.019,NA,12.298,2484.81888060086,0.008,7.212,NA,2.166,NA,NA,14.632,NA,0.024,0.091,20.987,0.917,1.615,2.109,0.089,0.488,0.524,0.012,0.107,0.012,0.303,0.027,NA,1.59916272901704,0.337,12
"MEX027","MEX027","North America","Trans-Mexican Volcanic Belt","Mexico","Guanajuato","Penjamo","Penjamo-2","","10",10,"","Active","Convergent","Continental","Active Continental Margin",20.423,-101.75,"","Michoacán-Guanajuato Volcanic Field","Central TMVB","","Obsidian","""Obsidian from Penjamo can be found in a clear grey flow band streching over 8km, immediatly due west of its town namesake in Guanjuato, Mexico. The best exposures can be found near the La Golondrina dam shoreline, where there is copious amounts of tool working debris. There are also vast quantities of obsidian in the 'flows embedded in volcanic ash in some abandoned modern quarries on Mexico Highway 110 on the southern edge of Churipitzeo' (Cobean 2002).""","","""Literature suggests alternate names for this source include: Sierra de Penjamo (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Cobean, R. H. (2002). A World of Obsidian: The Mining and Trade of a Volcanic Glass in Ancient Mexico. Serie Arqueologia de Mexico. Mexico City: Intituto Nacional de Anthropologia e Historia/University of Pittsburgh.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34329.627,NA,37694.927,NA,NA,326.582,13870.64,0.015,120.556,NA,150.701,NA,NA,602.683,NA,0.291,5.249,42.973,45.256,101.402,49.406,2.095,13.804,12.498,0.799,8.251,1.177,16.485,1.745,NA,14.14,5.062,839.197,NA,2039.733,0.025,NA,7.528,2133.58658844002,0.00385692765649294,3.438,NA,4.504,NA,NA,68.8581240578609,NA,0.017,0.151,25.639,0.781,2.835,1.46,0.089,0.549,0.423,0.021,0.169,0.03,0.509,0.044,NA,1.57083438612719,0.458,15
"MEX034","MEX034","North America","Trans-Mexican Volcanic Belt","Mexico","Hidalgo","Sierra de Pachuca","Sierra de Pachuca-2","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",20.143,-98.751,"","","Eastern TMVB","High","Obsidian","""Pachuca obsidian is transparent green with a green-gold tint. The glass is of fine quality for tool making and contains very few inclusions (Doering 2002).""","""Pachuca was one of the earliest sources exploited in Central Mexico, with blades associated with mammoth kill sites in the Late Pleistocene (Doering 2002).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002. ; Cobean, R. H. (2002). A World of Obsidian: The Mining and Trade of a Volcanic Glass in Ancient Mexico. Serie Arqueologia de Mexico. Mexico City: Intituto Nacional de Anthropologia e Historia/University of Pittsburgh.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,38757.845,NA,41569.1,NA,NA,789.682,13993.209,0.154,120.144,NA,116.513,NA,NA,693.876,NA,0.14,2.012,36.467,63.049,145.755,66.316,2.551,15.727,15.15,2.502,8.627,1.239,18.091,3.101,NA,10.805,4.249,622.363,NA,1847.296,0.235,NA,16.529,290.027,0.01,3.667,NA,1.637,NA,NA,31.357,NA,0.016,0.031,15.826,2.237,4.644,3.209,0.094,1.59546292742923,0.39,0.065,0.229,0.027,0.459,0.300812773956235,NA,0.108,0.951,11
"MEX035","MEX035","North America","Trans-Mexican Volcanic Belt","Mexico","Hidalgo","Sierra de Pachuca","Sierra de Pachuca-3","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",20.143,-98.751,"","","Eastern TMVB","Medium","Obsidian","""Pachuca obsidian is transparent green with a green-gold tint. The glass is of fine quality for tool making and contains very few inclusions (Doering 2002).""","""Pachuca was one of the earliest sources exploited in Central Mexico, with blades associated with mammoth kill sites in the Late Pleistocene (Doering 2002).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002. ; Cobean, R. H. (2002). A World of Obsidian: The Mining and Trade of a Volcanic Glass in Ancient Mexico. Serie Arqueologia de Mexico. Mexico City: Intituto Nacional de Anthropologia e Historia/University of Pittsburgh.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36006.448,NA,39912.9,NA,NA,883.649,14072.367,0.05,139.885,NA,160.412,NA,NA,750.367,NA,0.249,3.078,28.57,42.096,105.789,43.943,2.554,17.491,12.669,1.439,11.194,1.622,21.956,4.592,NA,16.829,6.134,770.099,NA,2957.864,0.095,NA,48.598,303.436,0.011,8.707,NA,3.659,NA,NA,64.182,NA,0.021,0.077,9.945,2.483,5.087,3.399,0.046,1.114,1.21171567576308,0.03,0.245,0.034,0.746,0.105,NA,0.365,0.727671923872198,27
"MEX054","MEX054","North America","Trans-Mexican Volcanic Belt","Mexico","Jalisco","Navajas","Navajas Group General","","10",10,"","Active","Convergent","Continental","Active Continental Margin",20.504,-103.614,"","Volcan Primavera","Western TMVB","High","Obsidian","","""The Navajas source area is quite extensive. There are numerous depressions and pits that clearly indicate ancient mining activity. The largest prehistoric quarry located to date (30m in diameter and 6m deep) is here. An estimated 2000 cubic meters of artefact-quality obsidian could have been extracted from this single pit. Several mining tunnels were also identified with depths ranging up to 8m. Hammerstones are found with high frequency. On the highest hill, overlooking the valley floor and lower hills where the obsidian was mined, is the location of the Navajas ceremonial precinct consisting of a series of structures dating to the late Formative and early Classic periods (El Arenal and Ahualulco phases, 350 BC to AD 450). A number of small Post-Classic complexes dot the entire region. Obsidian from Navajas is of high quality and it was employed for a wide range of artefacts, including some use in the late Formative for jewelry making' (Glascock et al 2010).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Phil C. Weigand, Rodrigo Esparza López, Michael A. Ohnersorgen, Mauricio Garduño, Joseph B. Mountjoy, and J. Andrew Darling. Geochemical Characterisation of Obsidian in Western Mexico: the Sources in Jalisco, Nayarit, and Zacatecas. Crossing the Straits: Prehistoric Obsidian Source Exploitation in the North Pacific Rim, edited by Yaroslav V. Kuzmin and Michael D. Glascock. (2010) 201-208. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27600,NA,38780,NA,611103,195.6,6020,0.25,24.8,15,117.2,27.6,14,107.4,22,NA,NA,3.01,28.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12.3,4.6,400,NA,1613.17279836453,0.02,103,55.1832611206852,196.066017177982,0.01,4.27487373415292,1,2.30710678118655,3.1142135623731,3,8.84974746830583,5,NA,NA,0.04,0.3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.2,1,30
"MEX068","MEX068","North America","Trans-Mexican Volcanic Belt","Mexico","Michoacán","Zinapecuaro","Zinapecuaro Group General","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",19.738,-100.838,"","Los Azufres Region","Eastern TMVB","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Rivero-Torres, T. Calligaro, D. Tenorio, and M. Jimémez-Reyes. Characterization of archaeological obsidians from Lagartero, Chiapas Mexico by PIXE. Journal of Archaeological Science 35 (2008) 3168-3171. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23000,NA,42000,NA,581,205,10000,NA,43,19,192,21,28,150,18,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2000,NA,2000,NA,60,10,1000,NA,4,2,16,2,7,19,6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"MEX075","MEX075","North America","Trans-Mexican Volcanic Belt","Mexico","Puebla","Zaragoza","Zaragoza Oyamales subsource","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",19.652,-97.478,"","","Eastern TMVB","","Obsidian","""Zaragoza glass is opaque and dense black, may contain particulates, and exhibits lateral banding of dark-grey to black. The flows are several meters thick (Doering 2002).""","""Zaragoza obsidian was heavily exploited and used during the Formative Period, and it is common in lithic assemblages. Mines and workshops can be found in the southern deposits, while the northern ones appear untouched. The deposits near Oyamales represent the southernmost of these deposits (Doering 2002).""","""Literature suggests alternate names for this source include: Oyameles (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Jimenez, L. Cruz, D. Tenorio, and M. Jimenez Reyes. Caracterization por ANN de Muestras de Yacimientos de Obsidiana del Golfo de Mexico. Ciencia UANL 5, 3 (2002) 351-356. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27900,NA,39000,NA,NA,230,8700,0.9,NA,NA,163,NA,NA,NA,NA,NA,NA,505,44.6,78,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,21.4,NA,400,NA,1000,NA,NA,4,100,0.1,NA,NA,3,NA,NA,NA,NA,NA,NA,7,0.5,4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.2,NA,1
"MEX076","MEX076","North America","Trans-Mexican Volcanic Belt","Mexico","Puebla","Zaragoza","Zaragoza Gomez Sur subsource","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",19.758,-97.508,"","","Eastern TMVB","","Obsidian","""Zaragoza glass is opaque and dense black, may contain particulates, and exhibits lateral banding of dark-grey to black. The flows are several meters thick (Doering 2002).""","""Zaragoza obsidian was heavily exploited and used during the Formative Period, and it is common in lithic assemblages. Mines and workshops can be found in the southern deposits, while the northern ones appear untouched (Doering 2002).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Knight, Charles L. F., Heng Hu, Michael D. Glascock, and Stephen A. Nelson. Obsidian Sub-Sources at the Zaragoza-Oyameles Quarry in Puebla, Mexico: Similarities with Altotonga and Their Distribution Throughout Mesoamerica. Latin American Antiquity 28, 1 (2017) 46-65. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29473.4666666667,NA,37556.35,NA,678.471428571429,289.857,8536.41428571429,NA,63.2285714285714,16.9571428571429,154.285714285714,4.68571428571429,37.7857142857143,176.971428571429,30.3,NA,NA,116.193333333333,NA,NA,NA,NA,5.34623333333333,NA,NA,NA,NA,NA,NA,NA,15.6714285714286,NA,277.093077021662,NA,2732.37919942391,NA,66.172444272162,65.8398545377764,288.559245381669,NA,12.8410428296296,1.67018675887573,6.89937885402944,0.929925752284506,9.25156357441425,30.7855872276684,10.8940350651171,NA,NA,10.5352756648003,NA,NA,NA,NA,0.16579361668452,NA,NA,NA,NA,NA,NA,NA,1.41151725188924,NA,10
"MEX077","MEX077","North America","Trans-Mexican Volcanic Belt","Mexico","Puebla","Zaragoza","Zaragoza Potreros Caldera subsource","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",19.684,-97.546,"","","Eastern TMVB","","Obsidian","""Zaragoza glass is opaque and dense black, may contain particulates, and exhibits lateral banding of dark-grey to black. The flows are several meters thick (Doering 2002).""","""Zaragoza obsidian was heavily exploited and used during the Formative Period, and it is common in lithic assemblages. Mines and workshops can be found in the southern deposits, while the northern ones appear untouched (Doering 2002).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Knight, Charles L. F., Heng Hu, Michael D. Glascock, and Stephen A. Nelson. Obsidian Sub-Sources at the Zaragoza-Oyameles Quarry in Puebla, Mexico: Similarities with Altotonga and Their Distribution Throughout Mesoamerica. Latin American Antiquity 28, 1 (2017) 46-65. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30050.45,NA,222032.85,NA,NA,250.285,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,400.475,NA,NA,NA,NA,4.21615,NA,NA,NA,NA,NA,NA,NA,NA,NA,433.951431614185,NA,258221.183643025,NA,NA,3.93858477120906,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,14.7856027946107,NA,NA,NA,NA,0.170200602231602,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"MEX086","MEX086","North America","Trans-Mexican Volcanic Belt","Mexico","Hidalgo","Sierra de Pachuca","Sierra de Pachuca Group General","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",20.143,-98.751,"","","Eastern TMVB","High","Obsidian","""Pachuca obsidian is transparent green with a green-gold tint. The glass is of fine quality for tool making and contains very few inclusions (Doering 2002).""","""Pachuca was one of the earliest sources exploited in Central Mexico, with blades associated with mammoth kill sites in the Late Pleistocene (Doering 2002).""","""Literature suggests alternate names for this source include: Cerro del las Navajas, Cerro de Minillas, Cerro Pelon, Cruz del Milagro, El Chapulin, El Ocote, Huasca, Pachuca Rancho, Guajalote, Sierra de las Navajas (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Smith, Michael E., Adrian L. Burke, Timothy S. Hare, and Michael D. Glascock. Sources of Imported Obsidian at Postclassic Sites in the Yautepec Valley, Morelos: A Characterization Study Using XRF and INAA. Latin American Antiquity 18, 4 (2007) 429-450. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,38960,NA,32919.9166666667,NA,140,1057.3,14086,1.7,234.6,26,224.454545454545,2.33333333333333,106.555555555556,955.1,85.4,NA,NA,8.22222222222222,42,97.8,NA,NA,16.5825,NA,NA,NA,NA,NA,NA,29.8,24.39,NA,3440.47860156412,NA,27710.4403836728,NA,2.63528395185915,219.858790233961,4405.51457374814,0.01,48.3960208208776,2,23.956644160696,0.887298334620742,4.8553439962742,77.1986265147652,4.81023769411698,NA,NA,7.91798234681313,5,0.1,NA,NA,1.38581804962508,NA,NA,NA,NA,NA,NA,0.836660026534076,2.73455419827138,NA,15
"MEX087","MEX087","North America","Trans-Mexican Volcanic Belt","Mexico","Puebla","Zaragoza","Zaragoza Group General","","10",10,"","Active","Convergent","Continental","Active Continental Margin",19.758,-97.507,"","","Eastern TMVB","","Obsidian","""Zaragoza glass is opaque and dense black, may contain particulates, and exhibits lateral banding of dark-grey to black. The flows are several meters thick (Doering 2002).""","""Zaragoza obsidian was heavily exploited and used during the Formative Period, and it is common in lithic assemblages. Mines and workshops can be found in the southern deposits, while the northern ones appear untouched (Doering 2002).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ebert, C.E., M. Dennison, K.G. Hirth, S.B. McClure, and D.J. Kennett. Formative Period Obsidian Exchange Along the Pacific Coast of Mesoamerica. Archaeometry 57, 1 (2015) 54-73. ; Pool, Christopher A; Knight, Charles L F, and Glascock, Michael D. Formative Obsidian Procurement at Tres Zapotes, Veracruz, Mexico: Implications for Olmec and Epi-Olmec Political Economy. Ancient Mesoamerica 25 (2014) 271-293. ; Smith, Michael E., Adrian L. Burke, Timothy S. Hare, and Michael D. Glascock. Sources of Imported Obsidian at Postclassic Sites in the Yautepec Valley, Morelos: A Characterization Study Using XRF and INAA. Latin American Antiquity 18, 4 (2007) 429-450. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29333.3333333333,NA,40193,NA,865.333333333333,244.5,9714.6,NA,53,28.6,70.6,90,31.6,96,119.2,15.3333333333333,NA,424.333333333333,NA,NA,NA,NA,4.96333333333333,NA,NA,NA,NA,NA,NA,NA,20,NA,288.675134594813,NA,1928.51092815156,NA,102.026140441229,11.9897060471861,1109.22552586413,NA,7.83333097723715,6.58519869337201,49.1453023698899,28.5929470116814,2.8228756555323,58.559167780655,49.6389761405398,0.577350269189626,NA,23.7135685491099,NA,NA,NA,NA,0.494401995680978,NA,NA,NA,NA,NA,NA,NA,1,NA,8
"MEX088","MEX088","North America","Trans-Mexican Volcanic Belt","Mexico","Zacatecas","Huitzila","Huitzila Group General","","10",10,"","Active","Convergent","Continental","Active Continental Margin",21.211,-103.611,"","","Western TMVB","High","Obsidian","""Huitzila is high quality obsidian and is found in many colors - including 'rainbow' varieties. The source was heavily exploited during pre-Hispanic times (Glascock et al 2010).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Darling, J.A. and F.M. Hayashida. compositional Analysis of the Huitzila and La Lobera Obsidian Sources in the Southern Madre Occidental, Mexico. Journal of Radioanalytical and Nuclear Chemistry 196, 2 (1995) 245-254. ; Glascock, Michael D., Phil C. Weigand, Rodrigo Esparza López, Michael A. Ohnersorgen, Mauricio Garduño, Joseph B. Mountjoy, and J. Andrew Darling. Geochemical Characterisation of Obsidian in Western Mexico: the Sources in Jalisco, Nayarit, and Zacatecas. Crossing the Straits: Prehistoric Obsidian Source Exploitation in the North Pacific Rim, edited by Yaroslav V. Kuzmin and Michael D. Glascock. (2010) 201-208. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34087.7192982456,NA,37420.6106870229,NA,1047116,400.832061068702,16773.2824427481,0.04,114.69465648855,20,127.870229007634,3,64,573.229007633588,55,0.403,2.54,2.52,77.7824561403509,154,62.7,1.84,11.6,12.9,0.183,7.27,1.05,15.4,3.19,NA,14.1561403508772,3.43368421052632,248.780853557251,NA,983.190028269812,0.0261754385964912,116,55.7379943221984,299.683795655196,0.01,6.66591486086702,1,1.41179399334936,1,9,19.2069367465448,6,0.031,0.004,0.03,1.70382101035436,4,4.1,0.05,0.5,0.5,0.004,0.26,0.02,0.4,0.05,NA,0.135355339059327,0.112792150804018,131
"MEX089","MEX089","North America","Northern Mexico","Mexico","Chihuahua","Sierra Fresnal","Sierra Fresnal East","","",NA,"","Active","Convergent","Continental","Active Continental Margin",30.84,-107.768,"","","Western TMVB","","Obsidian","""Sierra Fresnal is located in northern Chihuahua, and can be found in secondary alluvial deposits for 70 km around (Dolan et al 2016).""","","""Literature suggests alternate names for this source includes Lago Fredrico, Laguna Azteca, Ojo Fredrico (Dolan et al 2017, Shackley 2002).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Sierra Fresnal. http://www.swxrflab.net//sierra_fresnal.htm. ; Dolan, Sean G., Michael E. Whalen, Paul E. Minnis, and Steen M. Shackley. Obsidian in the Casas Grandes World: Procurement, Exchange, and Interaction in Chihuahua, Mexico, CE 1200-1450. Journal of Archaeological Science 11 (2017) 555-567. ; Shackley, Steven M. Source Provenance of Archaeological Obsidian from Mimbres Mogollon Sites in the Cader Mountains, Southwest New Mexico. Archaeological Research Facility, UC Berkeley (2002).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1141,344.8,10292.9,NA,49.3333333333333,NA,295.1,40.4,64,168.6,36,NA,NA,248.777777777778,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27.2222222222222,38.7,NA,NA,NA,NA,NA,160.934078981979,43.137506238127,1490.23223022454,NA,4.9749371855331,NA,18.465884459968,1.95505043981536,4.16333199893227,4.4522154285504,2.74873708374511,NA,NA,35.0634345785527,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.092906420717,4.90011337737313,NA,10
"MEX090","MEX090","North America","Northern Mexico","Mexico","Chihuahua","Sierra Fresnal","Sierra Fresnal West","","",NA,"","Active","Convergent","Continental","Active Continental Margin",30.84,-107.768,"","","Western TMVB","","Obsidian","""Sierra Fresnal is located in northern Chihuahua, and can be found in secondary alluvial deposits for 70 km around (Dolan et al 2016).""","","""Literature suggests alternate names for this source includes Lago Fredrico, Laguna Azteca, Ojo Fredrico (Dolan et al 2017, Shackley 2002).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Sierra Fresnal. http://www.swxrflab.net//sierra_fresnal.htm. ; Dolan, Sean G., Michael E. Whalen, Paul E. Minnis, and Steen M. Shackley. Obsidian in the Casas Grandes World: Procurement, Exchange, and Interaction in Chihuahua, Mexico, CE 1200-1450. Journal of Archaeological Science 11 (2017) 555-567. ; Shackley, Steven M. Source Provenance of Archaeological Obsidian from Mimbres Mogollon Sites in the Cader Mountains, Southwest New Mexico. Archaeological Research Facility, UC Berkeley (2002).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1146.33333333333,315.333333333333,10412.6666666667,NA,46,NA,301.333333333333,42,65,163.333333333333,37.1666666666667,NA,NA,229,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25.1666666666667,41.1666666666667,NA,NA,NA,NA,NA,39.1135100274402,18.2062260412933,325.214800811197,NA,3.286335345031,NA,8.35862827661732,1.54919333848297,2.60768096208106,4.36653943835008,2.13697605664328,NA,NA,19.9799899899875,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.56255081250434,3.43025752191678,NA,6
"MEX091","MEX091","North America","Trans-Mexican Volcanic Belt","Mexico","Jalisco","Navajas","Navajas 1","","10",10,"","Active","Convergent","Continental","Active Continental Margin",20.504,-103.614,"","Volcan Primavera","Western TMVB","High","Obsidian","","""'The Navajas source area is quite extensive. There are numerous depressions and pits that clearly indicate ancient mining activity. The largest prehistoric quarry located to date (30m in diameter and 6m deep) is here. An estimated 2000 cubic meters of artefact-quality obsidian could have been extracted from this single pit. Several mining tunnels were also identified with depths ranging up to 8m. Hammerstones are found with high frequency. On the highest hill, overlooking the valley floor and lower hills where the obsidian was mined, is the location of the Navajo ceremonial precinct consisting of a series of structures dating to the late Formative and early Classic periods (El Arenal and Ahualulco phases, 350 BC to AD 450). A number of small Post-Classic complexes dot the entire region. Obsidian from Navajas is of high quality and it was employed for a wide range of artefacts, including some use in the late Formative for jewelry making' (Glascock et al 2010).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Phil C. Weigand, Rodrigo Esparza López, Michael A. Ohnersorgen, Mauricio Garduño, Joseph B. Mountjoy, and J. Andrew Darling. Geochemical Characterisation of Obsidian in Western Mexico: the Sources in Jalisco, Nayarit, and Zacatecas. Crossing the Straits: Prehistoric Obsidian Source Exploitation in the North Pacific Rim, edited by Yaroslav V. Kuzmin and Michael D. Glascock. (2010) 201-208. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,44500,NA,29600,NA,2330,1104,45850,0.128,252,24,154.5,9,134,940,112,0.55,3.4,48,92.6,194,80.6,3.19,20.2,17.5,2.64,10.6,1.49,23.8,6.21,NA,17.1,8.02,800,NA,3301.34559672906,NA,54,143.058657865101,3381.67568261897,0.006,12.3210678118655,1,5.01776695296637,2,19,40.0416305603426,8,0.01,0.01,7,0.8,2,2.5,0.02,0.8,0.2,0.02,0.2,0.01,0.2,0.04,NA,0.8,0.16,18
"MEX092","MEX092","North America","Trans-Mexican Volcanic Belt","Mexico","Jalisco","Navajas","Navajas 2","","10",10,"","Active","Convergent","Continental","Active Continental Margin",20.504,-103.614,"","Volcan Primavera","Western TMVB","High","Obsidian","","""The Navajas source area is quite extensive. There are numerous depressions and pits that clearly indicate ancient mining activity. The largest prehistoric quarry located to date (30m in diameter and 6m deep) is here. An estimated 2000 cubic meters of artefact-quality obsidian could have been extracted from this single pit. Several mining tunnels were also identified with depths ranging up to 8m. Hammerstones are found with high frequency. On the highest hill, overlooking the valley floor and lower hills where the obsidian was mined, is the location of the Navajo ceremonial precinct consisting of a series of structures dating to the late Formative and early Classic periods (El Arenal and Ahualulco phases, 350 BC to AD 450). A number of small Post-Classic complexes dot the entire region. Obsidian from Navajas is of high quality and it was employed for a wide range of artefacts, including some use in the late Formative for jewelry making' (Glascock et al 2010).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Phil C. Weigand, Rodrigo Esparza López, Michael A. Ohnersorgen, Mauricio Garduño, Joseph B. Mountjoy, and J. Andrew Darling. Geochemical Characterisation of Obsidian in Western Mexico: the Sources in Jalisco, Nayarit, and Zacatecas. Crossing the Straits: Prehistoric Obsidian Source Exploitation in the North Pacific Rim, edited by Yaroslav V. Kuzmin and Michael D. Glascock. (2010) 201-208. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,46200,NA,33600,NA,2265,1197.5,41800,0.141,259.5,26,182.5,10,104,1051,108,0.62,3.99,85,107,225,88.1,3.69,23.2,19.4,3.33,12.1,1.69,28,7.56,NA,21.5,9.73,1000,NA,3196.32034355964,NA,104,133.111958724001,2697.05627484771,0.011,12.9246212024587,1,3.01776695296637,1,19,32.3418830920368,7,0.02,0.33919986979259,19,1,2,2.5,0.04,1.1,0.2,0.457297653363301,0.1,0.01,0.3,0.05,NA,0.2,0.45,10
"MEX093","MEX093","North America","Trans-Mexican Volcanic Belt","Mexico","Michoacán","Zinapecuaro","Zinapecuaro A","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",19.738,-100.838,"","","Central TMVB","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Espino, Denisse Argote, Jesus Sole, Pedro Lopez Garcia, and Osvaldo Sterpone Canuto. Análisis Composicional de Seis Yacimientos de Obsidiana del Centro Obsidiana del Centro de México y su Clasificación con DBSCAN. Arqueología 43 (2010) 198-216. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42.5,NA,197.5,6,44,114,15.5,NA,NA,35,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20,19,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.707106781186548,NA,2.12132034355964,1.28201458907021,5.4366374958198,1.4142135623731,0.707106781186548,NA,NA,3.85967795366266,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.4142135623731,1.4142135623731,NA,2
"MEX094","MEX094","North America","Trans-Mexican Volcanic Belt","Mexico","Michoacán","Zinapecuaro","Zinapecuaro B","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",19.738,-100.838,"","","Central TMVB","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Espino, Denisse Argote, Jesus Sole, Pedro Lopez Garcia, and Osvaldo Sterpone Canuto. Análisis Composicional de Seis Yacimientos de Obsidiana del Centro Obsidiana del Centro de México y su Clasificación con DBSCAN. Arqueología 43 (2010) 198-216. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42.5,NA,200.5,5,45,112,15.5,NA,NA,30.5,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20.5,18.5,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.707106781186548,NA,2.12132034355964,1.06834549089184,5.56019743890661,2.82842712474619,0.707106781186548,NA,NA,2.12132034355964,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.707106781186548,0.707106781186548,NA,2
"MEX095","MEX095","North America","Trans-Mexican Volcanic Belt","Mexico","Michoacán","Zinapecuaro","Zinapecuaro C","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",19.738,-100.838,"","","Central TMVB","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Espino, Denisse Argote, Jesus Sole, Pedro Lopez Garcia, and Osvaldo Sterpone Canuto. Análisis Composicional de Seis Yacimientos de Obsidiana del Centro Obsidiana del Centro de México y su Clasificación con DBSCAN. Arqueología 43 (2010) 198-216. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42,NA,193.5,5,43,112,15.5,NA,NA,39,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.5,18.5,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.4142135623731,NA,4.94974746830583,1.06834549089184,1.4142135623731,4.24264068711928,2.12132034355964,NA,NA,8.48528137423857,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.707106781186548,0.707106781186548,NA,2
"MEX099","MEX099","North America","Trans-Mexican Volcanic Belt","Mexico","Michoacán","Cerro Varal","Cerro Varal Group General",""," ",NA,"","Active","Convergent","Continental","Active Continental Margin",19.862,-101.768,"","Michoacán-Guanajuato Volcanic Field","Central TMVB","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Robert J. Speakman, and Helen P. Pollard. LA-ICP-MS as a Supplement to Abbreviated-INAA for Obsidian Artifacts from the Aztec-Tarascan Frontier. Chapter Three, Laser Ablation-ICP-MS in Archaeological Research, edited by Robert J. Speakman and Hector Neff, (2005) 28–38. University of New Mexico Press, Albuquerque.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36500,NA,NA,374,7050,0.49,35.3,NA,125,121,NA,140,NA,0.36,3.74,594,27.9,53,18.7,0.51,3.26,3.71,0.41,2.25,0.39,4.12,1.54,NA,11.7,3.65,NA,NA,4576.83126209968,0.05,NA,8,1084.43341103959,0.16,7.8,NA,2,27,NA,9,NA,0.02,0.06,28,0.5,0.9,2.5,0.03,0.19,0.06,0.056303915278965,0.1,0.01,0.12,0.03,NA,0.2,0.432996824606052,26
"UAK006","UAK006","North America","Beringia","USA","Alaska","Umnak","NE Umnak","","",NA,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",53.48472222,-168.1675,"","Aleutian Arc","","","Obsidian","""Obsidian from northeast Umnak Island is slightly hydrated microvesicular glass from a lava dome (Macdonald et al 1992).""","","","""Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34421.9425621168,542.724227763305,34533.8825427831,NA,1258.73810716074,697.005836082213,4126.56396768739,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5460.85057033831,88.4315511021639,4330.29460886269,NA,23.6938023813876,59.2288960961926,634.749480759189,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"UAK007","UAK007","North America","Beringia","USA","Alaska","Umnak","SW Umnak","","",NA,"Lava Dome","Active","Convergent","Continental","Active Continental Margin",53.1705555,-168.4,"","Aleutian Arc","","","Obsidian","","","","""Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,904.540379605508,32458.529024587,NA,779.218828242364,387.225464490118,1608.66052977644,0.9,20,NA,162,105,21,100,5.2,2.3,11.4,925,21,38,17,NA,NA,3,0.4,NA,0.27,3.4,0.55,22,15.5,7.2,NA,147.385918503606,4070.0605578493,NA,14.6675919503828,32.9049422756625,247.444712838328,0.231415659389576,2.9559739536744,NA,15.661508108781,22.4352553087287,2.59475880482308,11.4252640372901,0.725383314920616,0.172256167294256,0.969142485121686,102.005774489656,1.80572057906397,5.08400182501203,2.3142705170134,NA,NA,0.28693243565311,0.0549306490526488,NA,0.124516371473603,0.338404478060218,0.0533527977026537,3.50405377648384,1.7219188815397,0.854130722510568,2
"UAK009","UAK009","North America","Cascadia","USA","Alaska","Wrangell Mountains","Ptarnigan Lake","","",NA,"Lava Flow","Active","Convergent","Continental","Active Continental Margin",61.85,-141.183333,"","Wrangell Volcanic Belt","","","Obsidian","""Ptarnigan Lake obsidian comes from a lava flow on the northeast side of the lake, in the form of an Apache Tear (Macdonald et al 1992).""","","","""Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32048.0154888674,1206.05383947401,34699.9108242388,NA,1258.73810716074,387.225464490118,3916.73868119481,0.9,30,NA,109,100,14,157,14,0.7,3,670,25,36,16,NA,NA,3,0.38,NA,0.3,4.2,1.3,15,11.8,5.6,5084.24018617705,196.514558004808,4351.11333294376,NA,23.6938023813876,32.9049422756625,602.474083432451,0.231415659389576,4.4339609305116,NA,10.5376813818341,21.3669098178368,1.72983920321539,17.9376645385454,1.95295507863243,0.0524257900460779,0.255037496084654,73.8852636843995,2.14966735602854,4.81642278159035,2.17813695718908,NA,NA,0.28693243565311,0.0521841166000163,NA,0.138351523859559,0.41802906113321,0.126106612751727,2.38912757487534,1.31088018078507,0.664323895285997,2
"UAK010","UAK010","North America","Cascadia","USA","Alaska","Wrangell Mountains","Capitol Mountain","","",NA,"Lava Flow","Active","Convergent","Continental","Active Continental Margin",62.40027778,-144.040555,"","Wrangell Volcanic Belt","","","Obsidian","""Capitol Mountain obsidian is porphyritic, and from a strongly annealed section on the southeast lava flow (Macdonald et al 1992).""","","","""Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,39058.5188770571,2201.04825704007,30258.6542952992,NA,1948.0470706059,890.618568327272,5315.57392447868,0.4,54,NA,95,280,28,323,19,0.75,2.05,1077.5,40.5,74.5,31.5,NA,NA,5.6,1.09,NA,0.405,7.55,1.305,24.5,12.05,4.1,52.456872860499,127.921327255221,410.899032901225,NA,127.151750187325,54.761950357815,593.475531773253,0.102851404173145,2.82842712474619,NA,2.82842712474619,35.3553390593274,5.65685424949238,52.3259018078045,2.65043903528687,0.0707106781186548,0.353553390593274,10.6066017177982,3.53553390593274,4.94974746830583,2.12132034355964,NA,NA,0.14142135623731,0.0282842712474619,NA,0.0353553390593274,0.0707106781186545,0.0919238815542513,7.77817459305202,0.636396103067893,0.486379994762962,4
"UAZ013","UAZ013","North America","Colorado Plateau Transition Zone","USA","Arizona","San Francisco Peak","San Francisco Peak A","","15-7",11,"Pyroclastic Cone","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",35.319,-111.676,"","San Francisco Volcanic Field","","Poor","Obsidian","""San Francisco obsidian may be found in a large lava flow on the northwest slope. The glass is typically heavily vitrophric and contains interbanded ash layers, making it 'generally useless for biface manufacture' (Shackley 2005).""","","""Literature suggests alternate names for this source include: Fremont-Agassiz Saddle (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Sources of Archaeological Obsidian in the Greater American Southwest: An Update and Quantitative Analysis. American Antiquity 60, 3 (1995) 531-551. ; Peirce, H. W., P. E. Damon, and M. Shafiqullah. An Oligocene (?) Colorado Plateau Edge in Arizona. Technophysics 61 (1979) 1-24. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Shackley, Steven M. Obsidian: Geology and Archaeology in the North American Southwest. The University of Arizona Press. 2005.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,468,17651,NA,NA,NA,NA,138,4,81,753,143,NA,NA,43,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,50,24,506,NA,NA,NA,NA,6,3,5,27,5,NA,NA,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"UAZ014","UAZ014","North America","Colorado Plateau Transition Zone","USA","Arizona","San Francisco Peak","San Francisco Peaks B","","15-7",11,"Pyroclastic Cone","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",35.319,-111.676,"","San Francisco Volcanic Field","","","Obsidian","","","""Literature suggests alternate names for this source include: Fremont-Agassiz Saddle (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Roberts, Theodore M., Craig E. Skinner, and William D. Bryce. Hunter-gatherer Igneous Toolstone Procurement in Northern Arizona: A Geochemical Study of Projectile Points and Raw Material Sources. KIVA 80, 2 (2014) 193-212. ; Peirce, H. W., P. E. Damon, and M. Shafiqullah. An Oligocene (?) Colorado Plateau Edge in Arizona. Technophysics 61 (1979) 1-24. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32,786,26,228,36,NA,NA,961,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.5,99.6,2.8,24.5,4.5,NA,NA,40.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,21
"UCA012","UCA012","North America","Great Basin","USA","California","Casa Diablo","Casa Diablo Prospect Ridge subsource","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.581,-118.547,"","","Miocene Volcanism Arc Axes","Medium","Obsidian","""Casa Diablo is one of the largest sources of obsidian in the southwest, and is located in the Long Valley Caldera, California. There are between 16-26 subsources found over 65 square km, all of varying sizes and color. Obsidian here is primarily in the form of cobbles and boulders, reaching as large as one meter in length. Textures of Casa Diablo are glassy, but may exhibit fine-grained surfaces with occasional phenocryst inclusions (Giambastiani 2004).""","""There are four major outcrops used historically: Lookout Mountain, Dry Creek Canyon, Sawmill Ridge, and Obsidian Hill (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Casa Diablo, Hot Creek, Prospect Ridge (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Rick, Torben C., Craig E. Skinner, Jon M. Erlandson, and René L. Vellanoweth. Obsidian Source Characterization and Human Exchange Systems on California's Channel Islands. Pacific Coast Archaeological Society Quarterly 37, 3 (2001) 27-44. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29599.9031945789,603.026919737005,40842.9572380993,NA,659.339008512769,309.780371592095,2657.78696223934,0.4,NA,NA,123,NA,NA,NA,NA,1,3.5,NA,42,65,22,NA,NA,3.2,0.25,NA,0.23,4.2,1.66,NA,14.2,4.1,4695.86072751074,98.2572790024042,5121.40612394337,NA,12.4110393426316,26.3239538205301,408.821699472021,0.102851404173145,NA,NA,11.8911450455559,NA,NA,NA,NA,0.0748939857801112,0.297543745432096,NA,3.61144115812795,8.69631891120479,2.99493831613499,NA,NA,0.306061264696651,0.0343316556579055,NA,0.106069501625662,0.41802906113321,0.161028443975282,NA,1.57749987857186,0.486379994762962,2
"UCA016","UCA016","North America","Great Basin","USA","California","Coso","Coso: Joshua Ridge","","",NA,"Volcanic Field","Active","Convergent","Continental","Active Continental Margin",36.002,-117.809,"","Coso Volcanic Field","","Medium","Obsidian","""The Coso Volcanic Field lies in the Coso Range of California - and is the largest source of obsidian in eastern California, covering almost 80 square km. Obsidian from Coso Mountains typically has many vesicles, internal gas bubbles, and can appear 'foamy' depending on the size of the bubbles. Artifact-quality material can be found from the lag and colluvial deposits from flow breccia throughout the area (Giambastiani 2004).""","""Historically, the main source of the Coso Range has been Sugarloaf Mountain, but there are several notable primary sources: Cactus Peak, West Sugarloaf, and Joshua Ridge. There are also many secondary deposits with easy access, generally in the forms of cobbles and pebbles - while larger boulders can be found and mined. The clear and non-vesicular obsidian outcrops were most-often selected for tool production (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Coso, Coso Volcanic Field, Joshua Ridge, Joshua Ridge, Coso Volcanic Field (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Draucker, Anne Christine. Geochemical Characterization of Obsidian Subsources from the Coso Range, California Using Laser Ablation Inductively Coupled Plasma Mass Spectrometry as a Tool for Archaeological Investigations. California State University, Bakersfield (2007).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,968,510,12667,NA,271,52,212,11,29,396,87,NA,NA,68,NA,136,40,1.2,8,8,0.19,5,0.56,NA,NA,NA,NA,NA,NA,NA,NA,NA,62,30,685,NA,30,3,10,1,3,40,5,NA,NA,5,NA,10,4,0.13,1,1,0.02,0.45,0.06,NA,NA,NA,NA,NA,9
"UCA017","UCA017","North America","Great Basin","USA","California","Coso","Coso: Sugarloaf Mountain Group General","","",NA,"Volcanic Field","Active","Convergent","Continental","Active Continental Margin",36.022,-117.829,"","Coso Volcanic Field","","Medium","Obsidian","""The Coso Volcanic Field lies in the Coso Range of California - and is the largest source of obsidian in eastern California, covering almost 80 square km. Obsidian from Coso Mountains typically has many vesicles, internal gas bubbles, and can appear 'foamy' depending on the size of the bubbles. Artifact-quality material can be found from the lag and colluvial deposits from flow breccia throughout the area (Giambastiani 2004).""","""Historically, the main source of the Coso Range has been Sugarloaf Mountain, but there are several notable primary sources: Cactus Peak, West Sugarloaf, and Joshua Ridge. There are also many secondary deposits with easy access, generally in the forms of cobbles and pebbles - while larger boulders can be found and mined. The clear and non-vesicular obsidian outcrops were most-often selected for tool production (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Coso
Coso Volcanic Field, Sugarloaf, Sugarloaf Mountain, Sugarloaf East, Sugarloaf Southeast, Coso Volcanic Field (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Rick, Torben C., Craig E. Skinner, Jon M. Erlandson, and René L. Vellanoweth. Obsidian Source Characterization and Human Exchange Systems on California's Channel Islands. Pacific Coast Archaeological Society Quarterly 37, 3 (2001) 27-44. ; Draucker, Anne Christine. Geochemical Characterization of Obsidian Subsources from the Coso Range, California Using Laser Ablation Inductively Coupled Plasma Mass Spectrometry as a Tool for Archaeological Investigations. California State University, Bakersfield (2007).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,242,10,47.6666666666667,125.333333333333,43.3333333333333,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.80277563773199,4,2.26376261582597,5.52072594216369,2.04083299973307,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3
"UCA018","UCA018","North America","Great Basin","USA","California","Coso","Coso: West Cactus Peak","","",NA,"Volcanic Field","Active","Convergent","Continental","Active Continental Margin",36.078,-117.858,"","Coso Volcanic Field","","Medium","Obsidian","""The Coso Volcanic Field lies in the Coso Range of California - and is the largest source of obsidian in eastern California, covering almost 80 square km. Obsidian from Coso Mountains typically has many vesicles, internal gas bubbles, and can appear 'foamy' depending on the size of the bubbles. Artifact-quality material can be found from the lag and colluvial deposits from flow breccia throughout the area (Giambastiani 2004).""","""Historically, the main source of the Coso Range has been Sugarloaf Mountain, but there are several notable primary sources: Cactus Peak, West Sugarloaf, and Joshua Ridge. There are also many secondary deposits with easy access, generally in the forms of cobbles and pebbles - while larger boulders can be found and mined. The clear and non-vesicular obsidian outcrops were most-often selected for tool production (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Coso, Coso Volcanic Field, West Cactus Peak, West Cactus Peak, Coso Volcanic Field (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Draucker, Anne Christine. Geochemical Characterization of Obsidian Subsources from the Coso Range, California Using Laser Ablation Inductively Coupled Plasma Mass Spectrometry as a Tool for Archaeological Investigations. California State University, Bakersfield (2007).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,698.692307692308,548.5,11292.5384615385,NA,292.269230769231,59.8557692307692,295.461538461538,6.10576923076923,34.0192307692308,317.461538461538,111.903846153846,NA,NA,34.0288461538462,NA,88.9807692307692,29.2884615384615,1.15961538461538,8.57692307692308,7.38461538461539,0.0986538461538461,5.25,1.55230769230769,NA,NA,NA,NA,NA,NA,NA,NA,NA,72.7266461076996,32.9679139543962,985.601864015233,NA,54.4682084106781,8.93380426284682,42.538220524635,2.67191671745799,5.47742434733859,32.388205294076,16.4872993167054,NA,NA,15.3004438074845,NA,13.8562229286836,3.16037791311455,0.254985950399846,1.59828882451432,1.0719361394198,0.0245040957953392,0.747479644469027,1.91577074715132,NA,NA,NA,NA,NA,104
"UCA019","UCA019","North America","Great Basin","USA","California","Coso","Coso: West Sugarloaf","","",NA,"Volcanic Field","Active","Convergent","Continental","Active Continental Margin",36.0386,-117.83,"","Coso Volcanic Field","","Medium","Obsidian","""The Coso Volcanic Field lies in the Coso Range of California - and is the largest source of obsidian in eastern California, covering almost 80 square km. Obsidian from Coso Mountains typically has many vesicles, internal gas bubbles, and can appear 'foamy' depending on the size of the bubbles. Artifact-quality material can be found from the lag and colluvial deposits from flow breccia throughout the area (Giambastiani 2004).""","""Historically, the main source of the Coso Range has been Sugarloaf Mountain, but there are several notable primary sources: Cactus Peak, West Sugarloaf, and Joshua Ridge. There are also many secondary deposits with easy access, generally in the forms of cobbles and pebbles - while larger boulders can be found and mined. The clear and non-vesicular obsidian outcrops were most-often selected for tool production (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Coso, Coso Volcanic Field, West Sugarloaf, Coso Volcanic Field (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Draucker, Anne Christine. Geochemical Characterization of Obsidian Subsources from the Coso Range, California Using Laser Ablation Inductively Coupled Plasma Mass Spectrometry as a Tool for Archaeological Investigations. California State University, Bakersfield (2007). ; Rick, Torben C., Craig E. Skinner, Jon M. Erlandson, and René L. Vellanoweth. Obsidian Source Characterization and Human Exchange Systems on California's Channel Islands. Pacific Coast Archaeological Society Quarterly 37, 3 (2001) 27-44.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,272.5,10,54.6666666666667,144.5,47.5,NA,NA,18,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,11.1801416111082,4.77459666924148,2.86626010212795,6.39395922569756,2.88892496362074,NA,NA,15.302775637732,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"UCA040","UCA040","North America","California Ranges","USA","California","Los Guilicos","Los Guilicos A","","",NA,"","Active","Convergent","Continental","Active Continental Margin",38.418,-122.589,"","Sonoma Volcanic Field","","Medium","Obsidian","""Los Guilicos sources are found on the southern portion of Annadel State Park, California. Los Guilicos A is a 'dull, greasy luster and typically gray to gray-green color. This obsidian generally lacks any inclusions.' The nodules are very small, and there is no evidence of quarrying (Jackson 1989).""","","""Literature suggests alternate names for this source include: Guilicos A, Oakmont (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Jackson, Thomas L. Late Prehistoric Obsidian Production and Exchange in the North Coast Ranges, California. Contributions of the Archaeological Research Facility 48 (1989) 79-94.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,174,8,123,749,33,NA,NA,218,52,119,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,16.8216198205425,1.70935278542695,15.1978729996781,85.5752276393027,4.60339411391929,NA,NA,24.0402798256703,4.47130810053936,15.9209530835903,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12
"UCA041","UCA041","North America","California Ranges","USA","California","Los Guilicos","Los Guilicos B","","",NA,"","Active","Convergent","Continental","Active Continental Margin",38.418,-122.589,"","Sonoma Volcanic Field","","Poor","Obsidian","""Los Guilicos sources are found on the southern portion of Annadel State Park, California. Los Guilicos B obsidian typically exhibits 'a brilliant luster, numerous phenocrysts, and a black color in reflected light... Los Guilicos B has a very definite green color.' This variety is very small, and has little evidence of quarrying (Jackson 1989).""","","""Literature suggests alternate names for this source include: Guilicos B, Oakmont (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Jackson, Thomas L. Late Prehistoric Obsidian Production and Exchange in the North Coast Ranges, California. Contributions of the Archaeological Research Facility 48 (1989) 79-94.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,146,3,156,896,41,NA,NA,193,55,124,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,14.1146924930989,0.641007294535105,19.2753511215429,102.370365774119,5.7193684445664,NA,NA,21.2833670016255,4.72926818326279,16.5899006921445,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4
"UCA045","UCA045","North America","Great Basin","USA","California","Mono Glass Mountain","Mono Glass Mountain Group General","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.772,-118.708,"","Mono-Inyo Volcanic Field","Miocene Volcanism Arc Axes","Low","Obsidian","""Mono Glass Mountain obsidian deposits can be found at the crest of Glass Mountain, at an elevation of 3390 m asl, northeast of Long Valley, California. To the west lies the Glass Mountain Ridge, a steep-sided formation at the northern edge of the caldera. Due to a past eruption, secondary sources of obsidian can be found two to three miles out to the east and northeast of the ridge, while the alluvial outwash is composed of many cobbles of low-quality obsidian (Giambastiani 2004).""","""Mono Glass mountain obsidians come in a variety of forms, ranging from red, brown, mahogany, and black - with the occasional porphyritic nodules. Obsidian from the peak is described as a translucent black with black bands, as well as opaque blacks with white inclusions, with occasional lacy patterns, phenocrysts, and some mahogany varieties (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Glass Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hughes, Richard E. A New Look at Mono Basin Obsidians. Contributions of the Archaeological Research Facility, UC Berkeley 48 (1989) 1-12. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,501.5,344.95,5875.10802179222,NA,42.95,17.6,164.95,6.3,25.35,90.25,23.3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30.0503142810072,15.5415562191883,136.386436220176,NA,3.54391814845377,2.24514133563619,11.3381498469577,0.952435615946823,2.19919897350855,2.610411887186,2.19939117455492,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20
"UCA055","UCA055","North America","Great Basin","USA","California","Saline Range","Saline Range Variety 1","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",36.853,-117.675,"","","Miocene Volcanism Arc Axes","","Obsidian","""The Saline Range is composed of a volcanic tableland, separating the Saline Valley from Eureka Valley in California. The obsidian nodules found here are eroded out from rhyolitic flows and tuffs, mixing into alluvial deposits and transported as far away as 20 km. Primary outcrops for Saline Ranges 1, 2, and 3 can often be found in close proximity to each other on the east side of the ridge. The Queen Impostor source, Saline Valley 1, occurs in sizes ranging from pebbles to boulders. Obsidian sources here exhibit a high degree of translucency with a gold-brown cast, occasionally containing tight, parallel black banding - very similar in appearance to Truman-Queen glass, hence the name Queen Impostor (Giambastiani 2004).""","","""Literature suggests alternate names for this source include: Dry Mountain, Queen Impostor, Saline Valley 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,56.8,18.2,173.65,20,29.75,140.2,36,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7.10698051533946,4.56274169979695,5.40165042944955,1.87426406871193,1.89675144212722,6.84619407771256,1.98713203435596,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"UCA056","UCA056","North America","Great Basin","USA","California","Saline Range","Saline Range Variety 2","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",36.987,-117.658,"Location is Uncertain","","Miocene Volcanism Arc Axes","","Obsidian","""The Saline Range is composed of a volcanic tableland, separating the Saline Valley from Eureka Valley in California. The obsidian nodules found here are eroded out from rhyolitic flows and tuffs, mixing into alluvial deposits and transported as far away as 20 km. Primary outcrops for Saline Ranges 1, 2, and 3 can often be found in close proximity to each other on the east side of the ridge. Obsidian sources here exhibit a high degree of translucency with a gold-brown cast, occasionally containing tight, parallel black banding. Saline Ranges 2 and 3 often feature unpatterned and blotchy clouded areas (Giambastiani 2004).""","","""Literature suggests alternate names for this source include: Dry Mountain, Saline Valley 2""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Source Provenance of Obsidian Artifacts from the Spring Reserve, Las Vegas, Nevada. Archaeological Research Facility, UC Berkeley, 2011. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,259,10014,NA,52,NA,16,37,33,13,24,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24,22,NA,NA,NA,NA,NA,NA,22.0088316263459,1540.35690470219,NA,7.68553227955343,NA,1.54681561568207,7.90575663259963,4.07747812186485,8,3.3479229919413,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.82260411980055,2.44401389637894,NA,1
"UCA067","UCA067","North America","Great Basin","USA","California","Mono Glass Mountain","Mono Glass Mountain 1","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.772,-118.708,"","Mono-Inyo Volcanic Field","Miocene Volcanism Arc Axes","","Obsidian","""Mono Glass Mountain obsidian deposits can be found at the crest of Glass Mountain, at an elevation of 3390 m asl, northeast of Long Valley, California. To the west lies the Glass Mountain Ridge, a steep-sided formation at the northern edge of the caldera. Due to a past eruption, secondary sources of obsidian can be found two to three miles out to the east and northeast of the ridge, while the alluvial outwash is composed of many cobbles of low-quality obsidian (Giambastiani 2004).""","""Mono Glass mountain obsidians come in a variety of forms, ranging from red, brown, mahogany, and black - with the occasional porphyritic nodules. Obsidian from the peak is described as a translucent black with black bands, as well as opaque blacks with white inclusions, with occasional lacy patterns, phenocrysts, and some mahogany varieties (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Glass Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ;Eerkins, Jelmer W. and Michael D. Glascock. Northern Fish Lake Valley and the Volcanic Tablelands of Owens Valley: Two Minor Sources of Obsidian in the Western Great Basin. Journal of California and Great Basin Anthropology 22, 2 (2000) 331-342. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29081,NA,39060,NA,NA,278.8,5334,NA,29.5,NA,176.1,0,NA,136.9,NA,NA,NA,32.2,24.6,55.9,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.2,55.9,552,NA,1112,NA,NA,13,80.7,NA,4.3,NA,4.3,0,NA,10.9,NA,NA,NA,11.9,1.4,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.46,2,11
"UCA068","UCA068","North America","Great Basin","USA","California","Mono Glass Mountain","Mono Glass Mountain 2","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.772,-118.708,"","Mono-Inyo Volcanic Field","Miocene Volcanism Arc Axes","","Obsidian","""Mono Glass Mountain obsidian deposits can be found at the crest of Glass Mountain, at an elevation of 3390 m asl, northeast of Long Valley, California. To the west lies the Glass Mountain Ridge, a steep-sided formation at the northern edge of the caldera. Due to a past eruption, secondary sources of obsidian can be found two to three miles out to the east and northeast of the ridge, while the alluvial outwash is composed of many cobbles of low-quality obsidian (Giambastiani 2004).""","""Mono Glass mountain obsidians come in a variety of forms, ranging from red, brown, mahogany, and black - with the occasional porphyritic nodules. Obsidian from the peak is described as a translucent black with black bands, as well as opaque blacks with white inclusions, with occasional lacy patterns, phenocrysts, and some mahogany varieties (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Glass Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ;Eerkins, Jelmer W. and Michael D. Glascock. Northern Fish Lake Valley and the Volcanic Tablelands of Owens Valley: Two Minor Sources of Obsidian in the Western Great Basin. Journal of California and Great Basin Anthropology 22, 2 (2000) 331-342. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29581,NA,38732,NA,NA,353.5,5426,NA,32.2,NA,196.4,0,NA,147.1,NA,NA,NA,41.4,23.7,54.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,22,54.7,629,NA,901,NA,NA,11.9,179,NA,4.1,NA,5,0,NA,17.1,NA,NA,NA,6.7,0.53,0.96,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.44,0.96,5
"UCA069","UCA069","North America","Great Basin","USA","California","Mono Glass Mountain","Mono Glass Mountain 3","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.772,-118.708,"","Mono-Inyo Volcanic Field","Miocene Volcanism Arc Axes","","Obsidian","""Mono Glass Mountain obsidian deposits can be found at the crest of Glass Mountain, at an elevation of 3390 m asl, northeast of Long Valley, California. To the west lies the Glass Mountain Ridge, a steep-sided formation at the northern edge of the caldera. Due to a past eruption, secondary sources of obsidian can be found two to three miles out to the east and northeast of the ridge, while the alluvial outwash is composed of many cobbles of low-quality obsidian (Giambastiani 2004).""","""Mono Glass mountain obsidians come in a variety of forms, ranging from red, brown, mahogany, and black - with the occasional porphyritic nodules. Obsidian from the peak is described as a translucent black with black bands, as well as opaque blacks with white inclusions, with occasional lacy patterns, phenocrysts, and some mahogany varieties (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Glass Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ;Eerkins, Jelmer W. and Michael D. Glascock. Northern Fish Lake Valley and the Volcanic Tablelands of Owens Valley: Two Minor Sources of Obsidian in the Western Great Basin. Journal of California and Great Basin Anthropology 22, 2 (2000) 331-342. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28732,NA,40798,NA,NA,299.8,5158,NA,31.8,NA,162,0,NA,127.1,NA,NA,NA,28.5,23.6,54.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,16.8,54.1,1392,NA,1324,NA,NA,5.8,94,NA,4.69999858634229,NA,9.4,0,NA,14.5215105913957,NA,NA,NA,3.9,1.4,2.36,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.24,2.36,9
"UCA070","UCA070","North America","Great Basin","USA","California","Casa Diablo","Casa Diablo Group General","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.581,-118.547,"","","Miocene Volcanism Arc Axes","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Rick, Torben C., Craig E. Skinner, Jon M. Erlandson, and René L. Vellanoweth. Obsidian Source Characterization and Human Exchange Systems on California's Channel Islands. Pacific Coast Archaeological Society Quarterly 37, 3 (2001) 27-44. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,520,587,8010,NA,47.8705882352941,15.6764705882353,107.415789473684,98.5421052631579,16.9315789473684,96.521052631579,7.84210526315789,NA,NA,1315.88235294118,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,117,48,499,NA,3.5414081184139,2.19630795618794,24.2146667068232,6.91916368855389,1.14470904782784,42.6681812819902,4.0426655303103,NA,NA,151.79787657181,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19
"UCA071","UCA071","North America","Great Basin","USA","California","Coso","Coso Group General","","",NA,"Volcanic Field","Active","Convergent","Continental","Active Continental Margin",36.0386,-117.83,"","Coso Volcanic Field","","Medium","Obsidian","""The Coso Volcanic Field lies in the Coso Range of California - and is the largest source of obsidian in eastern California, covering almost 80 square km. Obsidian from Coso Mountains typically has many vesicles, internal gas bubbles, and can appear 'foamy' depending on the size of the bubbles. Artifact-quality material can be found from the lag and colluvial deposits from flow breccia throughout the area (Giambastiani 2004).""","""Historically, the main source of the Coso Range has been Sugarloaf Mountain, but there are several notable primary sources: Cactus Peak, West Sugarloaf, and Joshua Ridge. There are also many secondary deposits with easy access, generally in the forms of cobbles and pebbles - while larger boulders can be found and mined. The clear and non-vesicular obsidian outcrops were most-often selected for tool production (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Coso, Coso Volcanic Field, West Sugarloaf, Coso Volcanic Field (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Draucker, Anne Christine. Geochemical Characterization of Obsidian Subsources from the Coso Range, California Using Laser Ablation Inductively Coupled Plasma Mass Spectrometry as a Tool for Archaeological Investigations. California State University, Bakersfield (2007). ; Rick, Torben C., Craig E. Skinner, Jon M. Erlandson, and René L. Vellanoweth. Obsidian Source Characterization and Human Exchange Systems on California's Channel Islands. Pacific Coast Archaeological Society Quarterly 37, 3 (2001) 27-44. ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32864.0529202969,120.605383947401,36339.4401036137,NA,344.654481722584,147.145676506245,2640.30152169829,0.1,50.5,NA,252.2,166.95,56,98.6,30,0.875,6.6,8.73333333333333,17,38.25,22.5,NA,NA,5.925,0.045,NA,0.885,5.55,6.3125,32.75,32.05,13.375,1008.11865198147,19.6514558004808,1261.47810427977,NA,29.9699549323985,6.32336535608634,754.107136619881,0.0257128510432863,7.72442015083764,NA,28.1710718160338,95.7015057410971,10.6651513899117,5.75192250830182,2,0.05,0.522812904711937,3.75410886008029,1.4142135623731,1.70782512765993,2.38047614284762,NA,NA,1.0688779163216,0.0288675134594813,NA,0.170782512765993,0.58022983951764,0.614132179040745,4.57347424467075,2.59807621135331,1.1295279249905,9
"UCA073","UCA073","North America","Cascadia","USA","California","Paradise Ridge","Paradise Ridge 1","","42-0",21,"","Active","Convergent","Continental","Active Continental Margin",36.766,-121.637,"","","Cascade Arc","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hamusek-McGann, Blossom. The Tuscan Obsidian Source of Northern California: Archaeological Implications and Geochemical Variability. California State University, 1995. ; Madsen, J. K., D. J. Thorkelson, R. M. Friedman, and D. D. Marshall. Cenozoic to Recent Plate Configurations in the Pacific Basin: Ridge Subduction and Slab Window Magmatism in Western North America. Geosphere 2, 1 (2006) 11-34.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,752,363,8122,NA,49,13,110,65,16,92,10,NA,NA,532,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,132,35,724,NA,15,2,7,4,3,6,2,NA,NA,116,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,15
"UCA074","UCA074","North America","Cascadia","USA","California","Paradise Ridge","Paradise Ridge 2","","42-0",21,"","Active","Convergent","Continental","Active Continental Margin",36.766,-121.637,"","","Cascade Arc","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Hamusek-McGann, Blossom. The Tuscan Obsidian Source of Northern California: Archaeological Implications and Geochemical Variability. California State University, 1995. ; Madsen, J. K., D. J. Thorkelson, R. M. Friedman, and D. D. Marshall. Cenozoic to Recent Plate Configurations in the Pacific Basin: Ridge Subduction and Slab Window Magmatism in Western North America. Geosphere 2, 1 (2006) 11-34.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,832,353,8192,NA,32,15,115,70,18,109,11,NA,NA,11,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,153,34,642,NA,5,2,6,3,1,15,1,NA,NA,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12
"UID007","UID007","North America","Northern Rocky Mountains","USA","Idaho","Cannonball Mountain","Cannonball Mountain Group General","","",NA,"","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",43.464,-114.706,"","","","","Obsidian","","","""Literature suggests alternate names for this source may include Liberal Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Skinner, Craig E. and Jennifer J. Thatcher. X-Ray Fluorescence Analysis of Artifact Obsidian from the Craters of the Moon National Monument and Preserve, Butte and Blaine Counties, Idaho. Northwest Research Obsidian Studies Laboratory Report 2009-75.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,201,NA,368,8,113,1009,115,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,49,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,16,NA,5,9,4,8,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6,NA,NA,1
"UID021","UID021","North America","Columbia Plateau","USA","Idaho","Jasper Flats","Jasper Flats 1","","",NA,"","Active","Convergent","Continental","Active Continental Margin",43.372,-114.111,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; James, Malcom A., Jeff Bailey, and John M. D'Auria. A Volcanic Glass Library for the Pacific Northwest: Problems and Prospects. Canadian Journal of Archaeology 20 (1996) 93-122.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.942,0.009,NA,0.148,0.096,0.115,0.215,0.099,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.072,0.001,NA,0.004,0.006,0.004,0.005,0.005,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"UID022","UID022","North America","Columbia Plateau","USA","Idaho","Jasper Flats","Jasper Flats 2","","",NA,"","Active","Convergent","Continental","Active Continental Margin",43.372,-114.111,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; James, Malcom A., Jeff Bailey, and John M. D'Auria. A Volcanic Glass Library for the Pacific Northwest: Problems and Prospects. Canadian Journal of Archaeology 20 (1996) 93-122.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.171,0.011,NA,0.175,0.069,0.134,0.215,0.116,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.078,0.001,NA,0.003,0.002,0.007,0.009,0.004,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"UID047","UID047","North America","Columbia Plateau","USA","Idaho","Cannonball Mountain","Cannonball Mountain 1","","",NA,"","Active","Convergent","Continental","Active Continental Margin",43.464,-114.706,"","","","","Obsidian","","","""Literature suggests alternate names for this source may include Liberal Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Black, Marielle Loryn Pedro. Using X-Ray Fluorescence Spectrometry to Assess Variance in Obsidian Source Distribution in Southern Idaho. Boise State University, 2014. ; Kaiser, Bruce Personal Communication 2017.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,37964.875,NA,978,465.5,24272.9,NA,217.4,25.5,341.4,3.2,115.5,1034.8,117.7,NA,NA,3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,59,41.8,NA,NA,NA,1291.84667793268,NA,108,48.8684175309801,2445.45501208646,NA,11.2996913462633,2.72894501037256,15.3888106412395,2.03668393770792,3.43438920029599,33.6099291513514,4.02843420241472,NA,NA,5,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7,3.61463629715286,NA,10
"UID048","UID048","North America","Columbia Plateau","USA","Idaho","Cannonball Mountain","Cannonball Mountain 2","","",NA,"","Active","Convergent","Continental","Active Continental Margin",43.464,-114.706,"","","","","Obsidian","","","""Literature suggests alternate names for this source may include Liberal Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Black, Marielle Loryn Pedro. Using X-Ray Fluorescence Spectrometry to Assess Variance in Obsidian Source Distribution in Southern Idaho. Boise State University, 2014. ; Kaiser, Bruce Personal Communication 2017.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,35727.5,NA,NA,635.333333333333,32074.6666666667,NA,267.666666666667,25.6666666666667,312.666666666667,4.66666666666667,109.666666666667,675.333333333333,111.666666666667,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,38.3333333333333,NA,NA,NA,471.640223051427,NA,NA,93.3354363409003,2760.25278739349,NA,32.2507061977837,2.04083299973307,21.0041657989726,2.39296944860009,6.75320354932386,27.0983537421709,6.38675134594813,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.75830573921179,NA,3
"UID052","UID052","North America","Columbia Plateau","USA","Idaho","Blackfoot Volcanic Field","Blackfoot Volcanic Field North Cone","","",NA,"","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",42.8333,-111.5692777,"","Blackfoot Volcanic Field","","","Obsidian","","","",""" ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30861.0519522427,120.605383947401,36028.1370758843,NA,359.639459188783,464.670557388142,3077.4375352245,NA,50,NA,455,0.7,177,110,82,0.3,17.4,3,15,43,28,NA,NA,9.6,0.04,NA,2.29,6.1,9.94,42,50.1,33.6,4895.93499409642,19.6514558004808,4517.66312559232,NA,6.7696578232536,39.4859307307951,473.372494125498,NA,7.38993488418599,NA,43.9875690709589,0.149568368724858,21.870109926366,12.5677904410191,11.4387368891328,0.0224681957340334,1.47921747729099,0.330829538885371,1.28980041361712,5.75294943356625,3.81173967508089,NA,NA,0.918183794089951,0.00549306490526487,NA,1.05608329879463,0.607137445931567,0.96423056211705,6.68955720965096,5.5656861912993,3.98594337171599,2
"UID053","UID053","North America","Columbia Plateau","USA","Idaho","Blackfoot Volcanic Field","Blackfoot Volcanic Field Middle Cone","","",NA,"","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",42.82555556,-111.601111,"","Blackfoot Volcanic Field","","","Obsidian","","","",""" ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31157.7928363988,120.605383947401,37439.3774682577,NA,359.639459188783,542.115650286165,2797.67048656772,0.2,51,NA,460,0.3,173,106,90,0.5,18.6,9,17,45,30,NA,NA,10.1,0.04,NA,2.41,6.6,10.9,40,49.1,35.1,4943.01129211656,19.6514558004808,4694.62228028143,NA,6.7696578232536,46.0669191859275,430.338631023179,0.0514257020865725,7.53773358186971,NA,44.4709489508596,0.0641007294535105,21.3758701540187,12.1107798795275,12.5547112197799,0.0374469928900556,1.58123247572486,0.992488616656113,1.46177380209941,6.02052847698793,4.08400679472953,NA,NA,0.966005866698803,0.00549306490526487,NA,1.11142390833845,0.656902810352187,1.05735544537986,6.37100686633425,5.45459465055481,4.16388727223902,2
"UID054","UID054","North America","Columbia Plateau","USA","Idaho","Blackfoot Volcanic Field","China Hat","","",NA,"","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",42.80255556,-111.60861,"","Blackfoot Volcanic Field","","","Obsidian","","","",""" ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30564.3110680865,120.605383947401,37605.4057497134,NA,359.639459188783,542.115650286165,2727.72872440353,NA,48,NA,440,0.6,175,104,77,NA,19.1,2,21,59,35,NA,NA,10.3,0.03,NA,2.48,6.5,11.1,33,52.7,35,4848.85869607626,19.6514558004808,4715.4410043625,NA,6.7696578232536,46.0669191859275,419.5801652476,NA,7.09433748881855,NA,42.537429431257,0.128201458907021,21.6229900401924,11.8822745987817,10.7412529324784,NA,1.6237387250723,0.220553025923581,1.80572057906397,7.89358178093974,4.76467459385112,NA,NA,0.985134695742344,0.00411979867894866,NA,1.14370593057235,0.646949737468063,1.07675646272628,5.25608066472575,5.854524197235,4.15202434553748,2
"UNM020","UNM020","North America","Colorado Plateau Transition Zone","USA","New Mexico","No Agua Peaks","No Aqua Peaks North Hill","","3",3,"Volcanic Field","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",36.772,-105.78,"","San Antonio Mountains","","","Obsidian","","","""Literature suggests alternate names for this source include: Johns Manville Mine, No Agua Dome, No Agua North (IAOS World Source Catalog). (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Raymond Kunselmn, and Daniel Wolfman. Intrastructure Chemical Differentiation of Obsidian in the Jemez Mountains in the Taos Plateau, New Mexico. Journal of Archaeological Science 26 (1999) 861-868. ; Shackley, Steven M. The Taos Plateau Volcanic Field and No Agua Peak Obsidian. http://www.swxrflab.net//noaguapk.htm. ; Nielson, Dennis and Jeffrey B. Hulen. Internal Geology and Evolution of the Redondo Dome, Valles Caldera, New Mexico. Journal of Geophysical Research 89, B10 (1984) 8695-8711. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30300,NA,39400,NA,578,588,5471.81818181818,0.15,38,NA,130.454545454545,32.7272727272727,24,81.0909090909091,36,0.197,2.02,113,12,24.9,9.1,0.45,2.97,2.58,0.354,2.33,0.419,3.44,2.58,NA,9.3,2.9,400,NA,1600,0.02,111,12,1122.49877219173,0.012,7,NA,3.12628066332055,4.21222943446873,1,7.95983044134892,3,0.0147541151986819,0.02,7,0.2,3.33135909059999,0.3,0.01,0.22,0.04,0.0486136244115941,0.05,0.011,0.04,0.03,NA,0.1,0.1,17
"UNM021","UNM021","North America","Colorado Plateau Transition Zone","USA","New Mexico","No Agua Peaks","No Aqua Peaks West Hill","","3",3,"Volcanic Field","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",36.727,-105.907,"","San Antonio Mountains","","","Obsidian","","","""Literature suggests alternate names for this source include: Grefco Mine, No Agua Dome, No Agua West (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Raymond Kunselmn, and Daniel Wolfman. Intrastructure Chemical Differentiation of Obsidian in the Jemez Mountains in the Taos Plateau, New Mexico. Journal of Archaeological Science 26 (1999) 861-868. ; Shackley, Steven M. The Taos Plateau Volcanic Field and No Agua Peak Obsidian. http://www.swxrflab.net//noaguapk.htm. ; Nielson, Dennis and Jeffrey B. Hulen. Internal Geology and Evolution of the Redondo Dome, Valles Caldera, New Mexico. Journal of Geophysical Research 89, B10 (1984) 8695-8711. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34000,NA,37800,NA,NA,1200,3750,0.069,64,NA,285,9,54,109.818181818182,90,0.51,5.58,30.1818181818182,10.6,25.3,11.2,1.12,7.05,4.78,0.13,5.1,0.91,5.08,6.5,NA,21.8,6.9,1200,NA,1000,0.2,NA,30,70,0.01,3,NA,9.5509018657793,1,1,12.1166846908413,1,0.02,0.474369742717457,13.601479064516,0.1,0.3,1.52469587003236,0.09,0.16,0.05,0.004,0.05,0.03,0.08,0.09,NA,0.3,0.818541942405961,17
"UNM041","UNM041","North America","Colorado Plateau Transition Zone","USA","New Mexico","Antelope Wells","Antelope Creek East","","17.7",17.7,"Volcanic Field","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",35.386,-108.616,"","Zuni-Bandera Volcanic Field","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Mule Creek Regional Source, Western New Mexico. http://www.swxrflab.net//mulecr.htm. ; Condit, Christopher D., L. S. Crumpler, Jayne C. Aubele, and Wolfgang E. Elston. Patterns of Volcanism Along the Southern Margin of the Colorado Plateau: The Springerville Field. Journal of Geophysical Research 94, B6 (1989) 7975-7986. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,362.571428571429,NA,NA,NA,NA,246.095238095238,15.6190476190476,42.0476190476191,121.52380952381,26.8571428571429,NA,NA,79.8095238095238,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,37.8491366197056,NA,NA,NA,NA,14.5427121332465,2.81915218596284,3.62596456789349,7.01155508870213,3.08683841957616,NA,NA,4.79446605597586,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,21
"UNM042","UNM042","North America","Colorado Plateau Transition Zone","USA","New Mexico","Antelope Creek","Antelope Creek West","","17.7",17.7,"Volcanic Field","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",35.544,-108.963,"","Zuni-Bandera Volcanic Field","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Mule Creek Regional Source, Western New Mexico. http://www.swxrflab.net//mulecr.htm. ; Roth, Karen. Geochemical Variability of Obsidian in Western New Mexico with Laboratory-Based pXRF. Washington and Lee University, 2014. ; Condit, Christopher D., L. S. Crumpler, Jayne C. Aubele, and Wolfgang E. Elston. Patterns of Volcanism Along the Southern Margin of the Colorado Plateau: The Springerville Field. Journal of Geophysical Research 94, B6 (1989) 7975-7986. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,494.208333333333,10818,NA,84.2,20.7,257.125,17.0416666666667,44.375,120.416666666667,30.2083333333333,NA,NA,71.1785714285714,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31.6,NA,NA,NA,NA,NA,NA,166.930336724157,3654.72330614021,NA,10.3150375665821,0.823272602348565,29.9583950635312,4.57288004260531,6.58596993615975,23.3999566455687,5.66437506946143,NA,NA,3.01028456907535,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.95145914949049,NA,24
"UNM047","UNM047","North America","Colorado Plateau Transition Zone","USA","New Mexico","Antelope Creek","Antelope Creek Group General","","17.7",17.7,"Volcanic Field","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",35.544,-108.963,"","Zuni-Bandera Volcanic Field","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Roth, Karen. Geochemical Variability of Obsidian in Western New Mexico with Laboratory-Based pXRF. Washington and Lee University, 2014. ; Condit, Christopher D., L. S. Crumpler, Jayne C. Aubele, and Wolfgang E. Elston. Patterns of Volcanism Along the Southern Margin of the Colorado Plateau: The Springerville Field. Journal of Geophysical Research 94, B6 (1989) 7975-7986. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,599.2,8979,NA,85.4,20.3,299.7,12.3,52.6,142.1,35.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32.3,NA,NA,NA,NA,NA,NA,48.7711207808701,281.172940060423,NA,7.69126488658111,0.674948557710553,6.09280085200741,0.823272602348565,2.06559111797729,3.28125992061992,0.843274042711568,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.88856206322871,NA,10
"UNV021","UNV021","North America","Great Basin","USA","Nevada","Devil Peak","Devil Peak East","65.5-2.6","",29.2,"Volcanic Dome","Active","Convergent","Continental","Active Continental Margin",35.696,-115.453,"","","","High","Obsidian","""The Devil Peak obsidian source is located in the southern Spring Mountains, Nevada.Obsidian occurs on both sides of the peak in perlite and vitrophyre, within a series of coalesced Tertiary domes of rhyolite. The east and west deposits are chemically distinct and 5 km apart (Haarklau et al 2005).""","""Manufacturing of both East and West varieties can be found on the peak and in the surrounding secondary deposits. Devil Peak West is thought to be a higher quality and larger nodule source of obsidian than the East. Devil Peak obsidian is a translucent black with occasional bubbles and banding (Haarklau et al 2005).""","""Literature suggests alternate names for this source include: Devil Peak (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Sources of Archaeological Obsidian in the Greater American Southwest: An Update and Quantitative Analysis. American Antiquity 60, 3 (1995) 531-551. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Shackley, Steven M. Devil Peak, Clark County, Nevada. http://www.swxrflab.net/devilpk.htm.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,645.530421052632,533.829473684211,8760.83117647059,NA,43.9,NA,196.426105263158,120.017894736842,28.9017894736842,115.595789473684,29.8771578947368,NA,NA,420.087368421053,76.0256,143.0612,NA,NA,NA,NA,NA,NA,NA,NA,NA,40.116,NA,NA,NA,NA,NA,NA,92.738449569843,104.784966654526,673.498429826364,NA,8.18657971996035,NA,11.0657706591171,20.6077342966911,2.60963541454882,12.915033573847,19.3338955828852,NA,NA,149.536925587201,15.036626873807,25.2660313742064,NA,NA,NA,NA,NA,NA,NA,NA,NA,4.41091782042485,NA,NA,95
"UNV022","UNV022","North America","Great Basin","USA","Nevada","Devil Peak","Devil Peak West","65.5-2.6","",29.2,"Volcanic Dome","Active","Convergent","Continental","Active Continental Margin",35.696,-115.453,"","","","High","Obsidian","""The Devil Peak obsidian source is located in the southern Spring Mountains, Nevada.Obsidian occurs on both sides of the peak in perlite and vitrophyre, within a series of coalesced Tertiary domes of rhyolite. The east and west deposits are chemically distinct and 5 km apart (Haarklau et al 2005).""","""Manufacturing of both East and West varieties can be found on the peak and in the surrounding secondary deposits. Devil Peak West is thought to be a higher quality and larger nodule source of obsidian than the East. Devil Peak obsidian is a translucent black with occasional bubbles and banding (Haarklau et al 2005).""","""Literature suggests alternate names for this source include: Devil Peak, Umpire (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. Devil Peak, Clark County, Nevada. http://www.swxrflab.net/devilpk.htm.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,815.252,538.179333333333,9975.722,NA,NA,NA,178.503333333333,251.399333333333,25.9053333333333,155.372666666667,23.0406666666667,NA,NA,876.1262,86.589,163.448,NA,NA,NA,NA,NA,NA,NA,NA,NA,40.648,NA,NA,NA,NA,NA,NA,100.819941494018,50.2955688855769,617.370732070401,NA,NA,NA,9.87754500056037,9.80819370778962,1.68361374373555,5.92172569764045,1.87844718039231,NA,NA,124.182747842616,11.760666506056,18.2930295164275,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.99040738660993,NA,NA,15
"UNV028","UNV028","North America","Great Basin","USA","Nevada","Kane Springs Wash Caldera","Kane Springs Wash Caldera Variety 1","","",NA,"Caldera","Active","Convergent","Continental","Active Continental Margin",37.221,-114.716,"","","","Medium","Obsidian","""The Kane Springs Wash Caldera has a complex eruption history, located in the Delmar Mountains of Nevada. The two artifact-grade obsidian sources occur in two separate intra caldera units of early and late moat rhyolites. These units are described as having a high silica content due to the melting of the caldera walls, and the late moat rhyolite (Variety 2) contains a higher concentration of both Ba and Sr compared to the early moat (Variety 1) (Haarklau et al 2005).""","""Nodules of tool quality obsidian range from 1 to 10 cm in diameter and are available from both primary sources, as well as a wide distribution of secondary sources in the Delmar Mountains. Kane Springs obsidian is an opaque black with no inclusions (Haarklau et al 2005).""","""Literature suggests alternate names for this source include: Delamar Mountains, Kane Springs C, Kane Springs Variety C, Kane Springs Wash Caldera Variety 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Rees, Margret N. Archaeological Inventory, Site Assessment, and Data Management, Lake Mead National Recreation Area (LAME) and Parashant National Monument (PARA), Annual Report for 2008. University of Nevada, Las Vegas (2008). ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,39415.5,NA,717.28,207.551724137931,8490.5,NA,52.5172413793103,20.75,219.266666666667,65.4,56.4,163.633333333333,39.9666666666667,NA,NA,48.1923076923077,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27.76,22.5,NA,NA,NA,1254.95564330643,NA,203.989453040852,34.972832339757,128.313418368202,NA,9.67226539236793,0.5,46.9442889257098,41.7450108507429,11.1531217034019,13.4375508137866,7.18997617397045,NA,NA,27.2463498351858,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6.082737172564,1,NA,30
"UNV029","UNV029","North America","Great Basin","USA","Nevada","Kane Springs Wash Caldera","Kane Springs Wash Caldera Variety 2 (Kane Springs)","","",NA,"Caldera","Active","Convergent","Continental","Active Continental Margin",37.241,-114.682,"","","","Medium","Obsidian","""The Kane Springs Wash Caldera has a complex eruption history, located in the Delmar Mountains of Nevada. The two artifact-grade obsidian sources occur in two separate intra caldera units of early and late moat rhyolites. These units are described as having a high silica content due to the melting of the caldera walls, and the late moat rhyolite (Variety 2) contains a higher concentration of both Ba and Sr compared to the early moat (Variety 1) (Haarklau et al 2005).""","""Nodules of tool quality obsidian range from 1 to 10 cm in diameter and are available from both primary sources, as well as a wide distribution of secondary sources in the Delmar Mountains. Kane Springs obsidian is an opaque black with no inclusions (Haarklau et al 2005).""","""Literature suggests alternate names for this source include: Kane Spring, Kane Springs, Kane Springs A, Kane Springs Variety A, Kane Springs Wash, Kane Springs Wash Caldera Variety 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Rees, Margret N. Archaeological Inventory, Site Assessment, and Data Management, Lake Mead National Recreation Area (LAME) and Parashant National Monument (PARA), Annual Report for 2008. University of Nevada, Las Vegas (2008). ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,785,260,NA,NA,35.5,NA,197.5,35,36.25,142.5,26,NA,NA,201,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23.5,NA,NA,NA,NA,NA,NA,154.585572775606,38.2657521530222,NA,NA,8.81632236012453,NA,7.5,6.91522945769824,2.93614066163451,7.59267638593623,1.20710678118655,NA,NA,28.8322510366134,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.84842275106824,NA,NA,4
"UNV041","UNV041","North America","Great Basin","USA","Nevada","Obsidian Butte","Obsidian Butte Variety 1","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.318,-116.86,"","","Miocene Volcanism Arc Axes","","Obsidian","""The Obsidian Butte Volcanic Complex contains several well known subsources, including Crow Spring, Silver Peak, the Montezuma Range, Shoshone Mountain, and Tempiute Mountain, as well as Obsidian Butte. Obsidian Butte is a black-brown and slightly translucent obsidian featuring distinct banding, spherulites, and phenocrysts (Haarklau et al 2005).""","""The Obsidian Butte Volcanic Center was commonly utilized for point manufacturing spanning the entire prehistory of the Great Basin and Mojave Desert (Haarklau et al 2005).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,397.666666666667,334,NA,NA,45.2857142857143,NA,164,15.2857142857143,25.8571428571429,160.571428571429,28.4285714285714,NA,NA,20.5714285714286,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,59.4285714285714,NA,NA,NA,NA,NA,NA,118.250140291674,62.2404609076896,NA,NA,8.81077676883985,NA,7.43139024560011,5.05634864026419,2.47590007294853,6.39909673946247,1.47775553860354,NA,NA,28.7259270913455,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,46.9724546222477,NA,NA,7
"UNV042","UNV042","North America","Great Basin","USA","Nevada","Obsidian Butte","Obsidian Butte Variety 2","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.311,-116.863,"","","Miocene Volcanism Arc Axes","","Obsidian","""The Obsidian Butte Volcanic Complex contains several well known subsources, including Crow Spring, Silver Peak, the Montezuma Range, Shoshone Mountain, and Tempiute Mountain, as well as Obsidian Butte. Obsidian Butte is a black-brown and slightly translucent obsidian featuring distinct banding, spherulites, and phenocrysts (Haarklau et al 2005).""","""The Obsidian Butte Volcanic Center was commonly utilized for point manufacturing spanning the entire prehistory of the Great Basin and Mojave Desert (Haarklau et al 2005).""","""Literature suggests alternate names for this source are: Airfield Canyon, Airfield Canyon, Obsidian Butte Area, Obsidian Butte Variety H-3, Sarcobatus Flat A, Sarcobatus Flats, Tolicha Wash, and may include White Rock Canyon (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,644.5,355.6,NA,NA,37.2,NA,165.4,55.4,22.6,125.6,21.8,NA,NA,267.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25.2,NA,NA,NA,NA,NA,NA,94.0042631869348,36.383574251242,NA,NA,6.85576411921994,NA,6.85455112926691,5.44868329805051,2.70646407139026,5.58433309344846,1.76491106406735,NA,NA,21.1218486246016,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4.48103920879045,NA,NA,10
"UNV043","UNV043","North America","Great Basin","USA","Nevada","Obsidian Butte","Obsidian Butte Variety 3","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.303,-116.846,"","","Miocene Volcanism Arc Axes","","Obsidian","""The Obsidian Butte Volcanic Complex contains several well known subsources, including Crow Spring, Silver Peak, the Montezuma Range, Shoshone Mountain, and Tempiute Mountain, as well as Obsidian Butte. Obsidian Butte is a black-brown and slightly translucent obsidian featuring distinct banding, spherulites, and phenocrysts (Haarklau et al 2005).""","""The Obsidian Butte Volcanic Center was commonly utilized for point manufacturing spanning the entire prehistory of the Great Basin and Mojave Desert (Haarklau et al 2005).""","""Literature suggests alternate names for this source are: Obsidian Butte, Obsidian Butte Area, Obsidian Butte Variety H-5, Sarcobatus Flat B, Sarcobatus Flats, and may include Tolicha Wash White Rock Canyon (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,698.5,337.5,NA,NA,39.6,NA,171,85.9,25,145.1,22.8,NA,NA,456.8,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23.7,NA,NA,NA,NA,NA,NA,67.2257196439042,28.7897299201544,NA,NA,5.84757558155454,NA,4.04124145231931,5.33166499665831,2.3498365855988,4.90336896233473,1.40676470058236,NA,NA,30.7286568747233,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.37537873571852,NA,NA,10
"UNV044","UNV044","North America","Great Basin","USA","Nevada","Obsidian Butte","Obsidian Butte Variety 4","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.327,-116.842,"","","Miocene Volcanism Arc Axes","","Obsidian","""The Obsidian Butte Volcanic Complex contains several well known subsources, including Crow Spring, Silver Peak, the Montezuma Range, Shoshone Mountain, and Tempiute Mountain, as well as Obsidian Butte. Obsidian Butte is a black-brown and slightly translucent obsidian featuring distinct banding, spherulites, and phenocrysts (Haarklau et al 2005).""","""The Obsidian Butte Volcanic Center was commonly utilized for point manufacturing spanning the entire prehistory of the Great Basin and Mojave Desert (Haarklau et al 2005).""","""Literature suggests alternate names for this source are: Obsidian Butte, Obsidian Butte Area, Obsidian Butte Variety H-5, and may include Sarcobatus Flat B White Rock Canyon (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,770,346.5,NA,NA,39.5,NA,165.8,104.3,23.9,161.2,21.8,NA,NA,601.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23.2,NA,NA,NA,NA,NA,NA,89.1602675074591,51.2340800935966,NA,NA,7.58152131085755,NA,5.59629438913631,7.0609243123008,2.05025246730731,5.51108041719978,1.23786478737262,NA,NA,26.667187487285,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.4203203194063,NA,NA,10
"UNV045","UNV045","North America","Great Basin","USA","Nevada","Obsidian Butte","Obsidian Butte Variety 5","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.366,-116.866,"","","Miocene Volcanism Arc Axes","","Obsidian","""The Obsidian Butte Volcanic Complex contains several well known subsources, including Crow Spring, Silver Peak, the Montezuma Range, Shoshone Mountain, and Tempiute Mountain, as well as Obsidian Butte. Obsidian Butte is a black-brown and slightly translucent obsidian featuring distinct banding, spherulites, and phenocrysts (Haarklau et al 2005).""","""The Obsidian Butte Volcanic Center was commonly utilized for point manufacturing spanning the entire prehistory of the Great Basin and Mojave Desert (Haarklau et al 2005).""","""Literature suggests alternate names for this source include: North Obsidian Butte, Obsidian Butte Area, Stonewall Canyon, Unknown C (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,899.3,357.8,NA,NA,34.7,NA,147.9,118.2,19.8,158.3,19.3,NA,NA,758.1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23.5,NA,NA,NA,NA,NA,NA,115.882159642293,41.6466824559255,NA,NA,8.41910284699433,NA,5.20112827331587,6.70856916979699,2.01639777949432,5.20049012542463,1.24721705904866,NA,NA,31.2360136227004,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.84466196843155,NA,NA,10
"UNV056","UNV056","North America","Great Basin","USA","Nevada","Rock Canyon","Rock Canyon I","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.01,-113.687,"Location is Uncertain","","Miocene Volcanism Arc Axes","","Obsidian","","","""Literature suggests alternate names for this source include: Clover Mountain, Variety 1, Unknown Type C (IAOS World Source Catalog). (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Shackley, Steven M. and Craig Skinner. Source Provenance of Obsidian Paleoindian and Early Archaic Artifacts from the Great Basin. Archaeology Research Facility, UC Berkeley, 2015. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42501.6666666667,NA,1239,381,10002.5,NA,46.25,19,144.5,90,26.25,190,21.5,NA,NA,1139,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.3333333333333,NA,NA,NA,940.985830569905,NA,23.3222629739535,44.2944691807002,2221.25707652221,NA,2.5,1,7.04745817062199,4.32049379893857,5.56027577253743,5.35412613473634,5.68624070307733,NA,NA,125.604948263479,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.15470053837925,NA,4
"UNV057","UNV057","North America","Great Basin","USA","Nevada","Rock Canyon","Rock Canyon II","","",NA,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Clover Mountain, Variety 2, Unknown Type B (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,41546,NA,NA,538,11750,NA,61,21,136,112,37,296,31,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20,NA,NA,NA,5209.56251000529,NA,NA,45.717186930402,1807.38901839931,NA,9.01572055870691,2.21528117267515,13.1479327332976,23.9309389959773,4.5717178942121,33.8187815503786,4.32440053125752,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.22183081488994,NA,1
"UNV066","UNV066","North America","Great Basin","USA","Nevada","Kane Springs Wash Caldera","Kane Springs Wash Caldera Group General","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.221,-114.716,"","","Miocene Volcanism Arc Axes","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Rees, Margret N. Archaeological Inventory, Site Assessment, and Data Management, Lake Mead National Recreation Area (LAME) and Parashant National Monument (PARA), Annual Report for 2008. University of Nevada, Las Vegas (2008). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,44.49,20.72,202.333333333333,37.0583333333333,40.0416666666667,160.65,28.6166666666667,NA,NA,258,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24.9333333333333,27.1666666666667,NA,NA,NA,NA,NA,NA,NA,NA,NA,5.31756848351849,3.2100029394451,6.92919696961221,7.5872310629546,4.07859085604165,11.5196290010161,3.52147843001704,NA,NA,11.4497474683058,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.42489823613278,2.86861084212034,NA,12
"UNV067","UNV067","North America","Great Basin","USA","Nevada","Meadow Valley Mountains Vitrophyre","Meadow Valley Mountains Vitrophyre A","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.101,-114.66,"","","Miocene Volcanism Arc Axes","","Obsidian","""Meadow Valley Mountain obsidian is a uniform opaque black that may contain phenocrysts, and is composed of four subsources (Haarklau et al 2005).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,701,200.5,NA,NA,31,NA,186,21.5,32,129.5,21.5,NA,NA,66,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20,NA,NA,NA,NA,NA,NA,198.399278298667,18.8033008588991,NA,NA,5.16421356237309,NA,2.70710678118655,4.85355339059327,3,3.85355339059327,0.853553390593274,NA,NA,25.4423881554251,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5.91421356237309,NA,NA,2
"UNV068","UNV068","North America","Great Basin","USA","Nevada","Meadow Valley Mountains Vitrophyre","Meadow Valley Mountains Vitrophyre B","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.101,-114.66,"","","Miocene Volcanism Arc Axes","","Obsidian","""Meadow Valley Mountain obsidian is a uniform opaque black that may contain phenocrysts, and is composed of four subsources (Haarklau et al 2005).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,901,209,NA,NA,59,NA,193,27,49,165,35,NA,NA,36,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,22,NA,NA,NA,NA,NA,NA,89,27,NA,NA,7,NA,4,9,3,7,1,NA,NA,34,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4,NA,NA,1
"UNV069","UNV069","North America","Great Basin","USA","Nevada","Meadow Valley Mountains Vitrophyre","Meadow Valley Mountains Vitrophyre C","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.101,-114.66,"","","Miocene Volcanism Arc Axes","","Obsidian","""Meadow Valley Mountain obsidian is a uniform opaque black that may contain phenocrysts, and is composed of four subsources (Haarklau et al 2005).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,890,190,NA,NA,47,NA,281,21,63,124,47,NA,NA,18,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25,NA,NA,NA,NA,NA,NA,89,27,NA,NA,7,NA,4,9,3,7,1,NA,NA,31,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9,NA,NA,1
"UNV070","UNV070","North America","Great Basin","USA","Nevada","Meadow Valley Mountains Vitrophyre","Meadow Valley Mountains Vitrophyre D","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.101,-114.66,"","","Miocene Volcanism Arc Axes","","Obsidian","""Meadow Valley Mountain obsidian is a uniform opaque black that may contain phenocrysts, and is composed of four subsources (Haarklau et al 2005).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,691,240,NA,NA,62,NA,418,4,83,118,56,NA,NA,0,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33,NA,NA,NA,NA,NA,NA,88,27,NA,NA,7,NA,4,9,3,7,1,NA,NA,31,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4,NA,NA,1
"UNV071","UNV071","North America","Great Basin","USA","Nevada","Double H","Double H Subsource 1","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",41.706,-118.064,"","","Miocene Volcanism Arc Axes","","Obsidian","""Double H Mountains obsidian is olive green and tool quality material (Moore 2009).""","","""Literature suggests alternate names for this source include: Double H, Double H Mountain, Double H Mountains, Whitehorse (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,194.214285714286,25.5571428571429,208.142857142857,6.92857142857143,92.8714285714286,501.057142857143,36.8714285714286,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,43.9428571428571,27.1714285714286,NA,NA,NA,NA,NA,NA,NA,NA,NA,6.67113501754957,4.13658585523534,4.92295719561745,4.47843914371733,1.95099295587415,9.10508227914973,2.19786147333805,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.82197608555609,2.98581080728568,NA,7
"UNV072","UNV072","North America","Great Basin","USA","Nevada","Double H","Double H Subsource 2","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",41.706,-118.064,"","","Miocene Volcanism Arc Axes","Medium","Obsidian","""Double H Mountains obsidian is olive green and tool quality material (Moore 2009).""","","""Literature suggests alternate names for this source include: Double H, Double H Mountain, Double H Mountains, Whitehorse (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,194.45,17.975,200.6,5.4,90.775,487.925,35.725,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42.4,27.125,NA,NA,NA,NA,NA,NA,NA,NA,NA,9.35203218457121,3.50681131815292,7.12030036282444,3.96526503540975,2.235414927656,11.264067244122,2.86321598563476,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.68147217281017,3.53365527476313,NA,4
"UNV073","UNV073","North America","Great Basin","USA","Nevada","Double H","Double H Subsource 3","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",41.706,-118.064,"","","Miocene Volcanism Arc Axes","Medium","Obsidian","""Double H Mountains obsidian is olive green and tool quality material (Moore 2009).""","","""Literature suggests alternate names for this source include: Double H, Double H Mountain, Double H Mountains, Whitehorse (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,189.277777777778,26.6333333333333,201.566666666667,5.93333333333333,89.5666666666667,476.488888888889,34.3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,40.1111111111111,24.8444444444444,NA,NA,NA,NA,NA,NA,NA,NA,NA,15.469017750772,4.0443000653997,8.87749227293948,4.09121255605927,3.44882661920102,16.4271629759027,3.09677264514858,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.87253745408265,3.80723702602256,NA,9
"UNV074","UNV074","North America","Great Basin","USA","Nevada","Double H","Double H Subsource 4","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",41.706,-118.064,"","","Miocene Volcanism Arc Axes","Medium","Obsidian","""Double H Mountains obsidian is olive green and tool quality material (Moore 2009).""","","""Literature suggests alternate names for this source include: Double H, Double H Mountain, Double H Mountains, Whitehorse (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,196,25.9888888888889,208.588888888889,5.73333333333333,94.6555555555556,499.122222222222,36.2444444444444,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,44.1333333333333,26.5111111111111,NA,NA,NA,NA,NA,NA,NA,NA,NA,7.339217779466,3.31302136340933,5.39635999967649,5.37768718736334,2.0333399787157,10.3798858099646,2.65314789814681,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.94528605797292,2.3601108914679,NA,9
"UNV075","UNV075","North America","Great Basin","USA","Nevada","Double H","Double H Subsource 5","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",41.706,-118.064,"","","Miocene Volcanism Arc Axes","Medium","Obsidian","""Double H Mountains obsidian is olive green and tool quality material (Moore 2009).""","","""Literature suggests alternate names for this source include: Double H, Double H Mountain, Double H Mountains, Whitehorse (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,181.033333333333,27,200.1,10.2833333333333,89.7166666666667,472.666666666667,35.55,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,41.3833333333333,23,NA,NA,NA,NA,NA,NA,NA,NA,NA,8.03638230495148,3.03634531768072,6.93764736713374,13.4071017665244,3.27113370156256,11.3986064523134,2.68642331706234,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.97042294461536,3.43944307100621,NA,6
"UOR051","UOR051","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes 1","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.54,-120.066,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Glass Buttes, Glass Buttes A (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30800,NA,NA,NA,NA,314,5580,0.18,39,NA,81,18,NA,110,NA,0.423,3,1110,24,52,23,1,8,6,0.5,5,0.8,4,0.8,NA,7,NA,500,NA,NA,0.08,NA,11,80,0.016,6,NA,1,6,NA,8,NA,0.018,0.04,16,1,1,3,0.08,0.3,0.09,0.01,0.1,0.01,0.09,0.01,NA,0.1,NA,110
"UOR052","UOR052","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes 2","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.541,-120.123,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Glass Buttes B (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32200,NA,NA,NA,NA,318,6490,0.338,42,NA,68,45,NA,140,NA,0.335,2,1250,37,75,31,1,7,7,1,5,0.7,5,0.7,NA,7,NA,300,NA,NA,0.05,NA,7,110,0.017,5,NA,1,9,NA,12,NA,0.02,0.04,17,1,1,4,0.09,0.3,0.1,0.01,0.2,0.01,0.06,0.01,NA,3.1,NA,26
"UOR053","UOR053","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes 3","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.554,-120.018,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Glass Buttes C, Juniper Spring, Variety 1, Little Glass Butte (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28300,NA,NA,NA,NA,327,6200,0.389,31,NA,95,78,NA,118,NA,0.205,4,1270,26,48,19,0.58,4,4,0.6,3,0.4,4,0.7,NA,8,NA,600,NA,NA,0.05,NA,6,100,0.013,7,NA,1,20,NA,7,NA,0.02,0.05,16,0.5,1,5,0.03,0.3,0.056,0.01,0.1,0.01,0.06,0.01,NA,0.1,NA,32
"UOR054","UOR054","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes 4","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.53,-119.975,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Glass Buttes D, Sand Flat (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746.Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30300,NA,NA,NA,NA,416,4700,0.071,55,NA,111,NA,NA,114,NA,0.47,5,259,18,75,22,1.5,10,7,0.2,7,1,4,1,NA,11,NA,500,NA,NA,0.1,NA,5,100,0.009,6,NA,2,NA,NA,8,NA,0.0352001733166523,0.08,15,0.5,1,7,0.07,0.4,0.1,0.007,0.3,0.02,0.1,0.02,NA,0.2,NA,28
"UOR055","UOR055","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes 5","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.554,-119.968,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Glass Buttes E, Potato Hills, Wise Flat (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,30900,NA,NA,NA,NA,447,4770,0.049,58,NA,121,NA,NA,108,NA,0.5,5,62,15,38,19,1.6,11,7,0.2,8,1,5,1,NA,12,NA,300,NA,NA,0.13,NA,4,100,0.0125992970112103,5,NA,2,NA,NA,10,NA,0.03,0.09,13,0.2,1,2,0.215847647145449,0.5,0.1,0.0274653245263244,0.1,0.012,0.1,0.02,NA,0.2,NA,12
"UOR056","UOR056","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes 6","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.53,-120.029,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Glass Buttes F, Little Glass Butte (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28800,NA,NA,NA,NA,358,5660,0.29,32,NA,105,48,NA,119,NA,0.2,4,1040,24,47,24,0.6,4,4,0.5,3,0.5,4,0.7,NA,9,NA,400,NA,NA,0.09,NA,6,120,0.011,6,NA,2,11,NA,8,NA,0.0149787971560223,0.09,19,0.4,1,5,0.03,0.2,0.06,0.01,0.1,0.009,0.08,0.0679035607124683,NA,0.2,NA,12
"UOR057","UOR057","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes 7","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.531,-120.112,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Juniper Spring, Variety 2, Midnight Ridge, Glass Buttes G (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ambroz, Jessica A, Glascock, Micheal D, and Skinner, Craig E. Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon. Journal of Archaeological Science (2001) 28, 741-746. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,32800,NA,NA,NA,NA,425,5350,0.172,49,NA,75,17,NA,104,NA,0.4,3,1000,21,46,20,1,8,5,0.7,6,0.8,4,0.9,NA,5,NA,200,NA,NA,0.06,NA,2,70,0.011,3,NA,1,3,NA,9,NA,0.03,0.03,27,0.6,1,2,0.14,0.4,0.2,0.006,0.4,0.02,0.07,0.005,NA,0.09,NA,5
"UOR059","UOR059","North America","","USA","Oregon","Glass Buttes","Glass Buttes 9","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.531,-120.112,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Skinner, Craig E. and Jennifer J. Thatcher. X-Ray Fluorescence Analysis and Obsidian Hydration Rim Measurement of Artifact Obsidian from the 34 Archaeological Sites Associated with the Proposed FTV Western Fiber Build Project, Deschutes, Lake, Harney, and Malheur Counties, Oregon. Northwest Research Obsidian Studies Laboratory Report 1998-56 (2003). ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,432,348.5,NA,NA,42.5,NA,107,11.5,58.5,95.5,13,NA,NA,581,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,18,NA,NA,NA,NA,NA,NA,8.48528137423857,4.94974746830583,NA,NA,3.53553390593274,NA,8.48528137423857,0.707106781186548,0.707106781186548,2.12132034355964,1.4142135623731,NA,NA,48.0832611206852,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.4142135623731,NA,NA,2
"UOR066","UOR066","North America","Columbia Plateau","USA","Oregon","Horse Mountain","Horse Mountain Variety 1","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.134,-120.158,"","","High Lava Plains","","Obsidian","""Horse Mountain is a vitrophyre dome that is densely surrounded by obsidian nodules for miles around (Moore 2009).""","","""Literature suggests alternate names for this source include: Horse Mountain Variety 1, Horse Mountain A, Poverty Flat, Poverty Basin (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Thatcher, Jennifer H. The Distribution of Geologic and Artifact Obsidian from the Silver Lake/Sycan Marsh Geochemical Source Group. South-Central Oregon. Oregon State University (2000). ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,638,341,12939.2260003757,NA,187,NA,132,5,102,620,40,NA,NA,45,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36,NA,NA,NA,NA,NA,NA,95,47,769.359383806124,NA,8,NA,3,7,3,7,2,NA,NA,13,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3,NA,NA,1
"UOR070","UOR070","North America","Columbia Plateau","USA","Oregon","Indian Creek Butte","Indian Creek Buttes A","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.136,-118.217,"","","High Lava Plains","","Obsidian","","","""Literature suggests an alternate name for this source is Indian Creek Buttes A Petroglyphs, Baker, Dooley Mountain, Wallowaand may include Big Gulch (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lyons, William H, Scott P. Thomas and Craig E. Skinner. Changing Obsidian Sources at the Lost Dune and McCoy Creek Sites, Blitzen Valley, Southeast Oregon. Journal of California and Great Basin Anthropology 23, 2 (2001) 273-296. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,57.0588235294118,17,178.960784313725,33,52.6274509803922,190.941176470588,35.7058823529412,NA,NA,205.235294117647,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,4.62386184479111,2.76929551764398,4.58636360003777,5.01535095085716,3.53849483827642,44.3560453358128,9.21115951166213,NA,NA,230.358191128532,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,51
"UOR071","UOR071","North America","Columbia Plateau","USA","Oregon","Indian Creek Butte","Indian Creek Buttes Variety B","","",NA,"","Active","Convergent","Continental","Active Continental Margin",43.136,-118.217,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Indian Creek Buttes B, Baker, Dooley Mountain, Wallowa, Beaver Mountain(IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lyons, William H, Scott P. Thomas and Craig E. Skinner. Changing Obsidian Sources at the Lost Dune and McCoy Creek Sites, Blitzen Valley, Southeast Oregon. Journal of California and Great Basin Anthropology 23, 2 (2001) 273-296.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,58,NA,188,18,57,147,34,NA,NA,171,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6,NA,5,2,3,4,2,NA,NA,20,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9
"UOR072","UOR072","North America","Cascadia","USA","Oregon","Inman Creek","Inman Creek A","","33",33,"","Active","Convergent","Continental","Active Continental Margin",44.118,-123.348,"","","","","Obsidian","""Inman Creek obsidian is widely distributed through alluvial means, and may be far from the outcrop. Inman Creek A has been identified at originating from Mount David Douglas, Oregon. Inman Creek B has yet to be located, but it is probably within the same vicinity. Creek B is characterized ass having lesser concentrations of Sr and Zr than Creek A (Skinner and Baxter 1997).""","","""Literature suggests alternate names for this source include: Bills Creek, Eagle Creek, Fern Ridge, Inman, Long Tom, Petite Creek, Pleasant Hill, Salt Creek, Staley Creek, Siuslaw River, Willamette River Gravels (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Skinner, Craig E. and Paul W. Baxter. Trace Element and Visual Characterization Studies of Obsidian from Sites 35-PO-15 and 35-PO-47, Willamette Valley, Western Oregon: An Archaeological Application of Atomic Absorption Spectrometry. 1997. ; Madsen, J. K., D. J. Thorkelson, R. M. Friedman, and D. D. Marshall. Cenozoic to Recent Plate Configurations in the Pacific Basin: Ridge Subduction and Slab Window Magmatism in Western North America. Geosphere 2, 1 (2006) 11-34.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,80.7307692307692,138.846153846154,NA,54.0769230769231,NA,NA,NA,775,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.23709977082279,4.97748778154046,NA,1.12864793175115,NA,NA,NA,28.8249891587144,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,26
"UOR073","UOR073","North America","Cascadia","USA","Oregon","Inman Creek","Inman Creek B","","33",33,"","Active","Convergent","Continental","Active Continental Margin",44.118,-123.348,"","","","","Obsidian","""Inman Creek obsidian is widely distributed through alluvial means, and may be far from the outcrop. Inman Creek A has been identified at originating from Mount David Douglas, Oregon. Inman Creek B has yet to be located, but it is probably within the same vicinity. Creek B is characterized ass having lesser concentrations of Sr and Zr than Creek A (Skinner and Baxter 1997).""","","""Literature suggests alternate names for this source include: Bills Creek, Eagle Creek, Fern Ridge, Inman, Long Tom, Mt. David Douglas, Petite Creek, Pleasant Hill, Siuslaw River, Staley Creek, Unknown D, Willamette River Gravels (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Skinner, Craig E. and Paul W. Baxter. Trace Element and Visual Characterization Studies of Obsidian from Sites 35-PO-15 and 35-PO-47, Willamette Valley, Western Oregon: An Archaeological Application of Atomic Absorption Spectrometry. 1997. ; Madsen, J. K., D. J. Thorkelson, R. M. Friedman, and D. D. Marshall. Cenozoic to Recent Plate Configurations in the Pacific Basin: Ridge Subduction and Slab Window Magmatism in Western North America. Geosphere 2, 1 (2006) 11-34.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,89.1428571428571,108.571428571429,NA,49.2857142857143,NA,NA,NA,765.285714285714,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.96808419852332,5.31843156256751,NA,0.755928946018454,NA,NA,NA,18.7324521060314,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7
"UOR129","UOR129","North America","Great Basin","USA","Oregon","Whitehorse","Whitehorse 1","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",42.108,-118.181,"Location is Questionable","","Miocene Volcanism Arc Axes","","Obsidian","","","""Literature suggests alternate names for this source include: Ankle Creek, Bretz Mine, Whitehorse Ranch (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lyons, William H, Scott P. Thomas and Craig E. Skinner. Changing Obsidian Sources at the Lost Dune and McCoy Creek Sites, Blitzen Valley, Southeast Oregon. Journal of California and Great Basin Anthropology 23, 2 (2001) 273-296. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,199,NA,210,6,90,503,11,NA,NA,11,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,29.4119408390603,NA,20.3019549558272,1.28201458907021,11.1203948778132,57.4690781075691,1.53446470463976,NA,NA,1.21304164257969,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1
"UOR137","UOR137","North America","Columbia Plateau","USA","Oregon","Horse Mountain","Horse Mountain Group General","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.14,-120.177,"","","High Lava Plains","","Obsidian","""Horse Mountain is a vitrophyre dome that is densely surrounded by obsidian nodules for miles around (Moore 2009).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Thatcher, Jennifer H. The Distribution of Geologic and Artifact Obsidian from the Silver Lake/Sycan Marsh Geochemical Source Group. South-Central Oregon. Oregon State University (2000). ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992). ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,35163.7947725073,NA,37190.3350460741,NA,1078.91837756635,619.560743184189,8602.83674619575,NA,195,NA,114,2,120,710,39,2.2,5.6,42,62,124,70,NA,NA,15.5,1.16,NA,1.65,15,2.36,32,12.5,4.9,5578.54131538871,NA,4663.39419415981,NA,20.3089734697608,52.6479076410601,1323.29129039628,NA,28.8207460483254,NA,11.0210612617348,0.427338196356737,14.8271931704176,81.1193746647595,5.44037486190462,0.164766768716245,0.476069992691354,4.63161354439519,5.33117504295078,16.5899006921445,9.52934918770223,NA,NA,1.4824842508744,0.159298882252681,NA,0.760933381227573,1.49296093261861,0.22893200468775,5.0968054930674,1.38864425930621,0.581283408375248,2
"UOR138","UOR138","North America","Columbia Plateau","USA","Oregon","Quartz Mountain","Quartz Mountain Group General","","2.6",2.6,"","Active","Convergent","Continental","Active Continental Margin",43.692,-121.185,"","Newberry Volcanic Field","Cascade Arc","High","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Thatcher, Jennifer H. The Distribution of Geologic and Artifact Obsidian from the Silver Lake/Sycan Marsh Geochemical Source Group. South-Central Oregon. Oregon State University (2000). ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33754.2755727654,301.513459868503,33454.6987133212,NA,562.819729594391,297.056366122529,8130.72985158745,0.4,66,NA,142.25,68.25,45.75,188,10.25,0.6,6.2,948.25,27,56,23,NA,NA,6.4,0.65,NA,0.65,5.5,1.07,26.25,11.5,4.4,5354.92889979295,49.1286395012022,4194.97290233574,NA,101.572357875109,54.7311566307036,2336.66372257559,0.102851404173145,7.12859017617954,NA,6.859959576962,5.29698822107065,2.53077640640442,11.0166481891865,1.47871355387817,0.0449363914680668,0.527077491908285,26.6723950129845,2.32164074451082,7.49221321580721,3.13107187595931,NA,NA,0.612122529393301,0.0892623047105542,NA,0.299761635029044,0.547419008626823,0.103795442803344,3.26443837104274,1.27755271856172,0.52196877486757,5
"UOR139","UOR139","North America","Columbia Plateau","USA","Oregon","Whitehorse","Whitehorse 2","","",NA,"","Active","Convergent","Continental","Active Continental Margin",42.108,-118.181,"Location is Questionable","","Cascade Arc","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lyons, William H, Scott P. Thomas and Craig E. Skinner. Changing Obsidian Sources at the Lost Dune and McCoy Creek Sites, Blitzen Valley, Southeast Oregon. Journal of California and Great Basin Anthropology 23, 2 (2001) 273-296.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,95,NA,195,4,67,473,33,NA,NA,6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9,NA,4,2,2,13,1,NA,NA,5,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5
"UOR148","UOR148","North America","Great Basin","USA","Oregon","Beatys Butte","Beatys Butte Group General","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",42.394,-119.324,"","","High Lava Plains","High","Obsidian","""Dense concentrations of surface nodules covering several square kilometers are found on the lower northern,
eastern, and western slopes of Beatys Butte and are common in the lacustrine deposits of Pluvial Lake Catlow
to the north and east of the butte. Obsidian from this source was widely used in the Steens Mountain area and
the southeastern portion of the state and has been identified as far north as the Malheur National Forest and as
far west as the southern Oregon coast' Skinner and Thatcher 2003).""","","""Literature suggests alternate names for this source include: Beaty's Butte, Beatty's Butte (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lyons, William H, Scott P. Thomas and Craig E. Skinner. Changing Obsidian Sources at the Lost Dune and McCoy Creek Sites, Blitzen Valley, Southeast Oregon. Journal of California and Great Basin Anthropology 23, 2 (2001) 273-296. ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992). ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,27522.7170054856,904.540379605508,40925.9713788271,NA,1018.97846770155,464.670557388142,2517.90343791095,0.9,34.8307692307692,NA,128.892307692308,174.969230769231,14.9538461538462,160.769230769231,11.0461538461538,0.4,2.8,965.307692307692,23,38,11,NA,NA,2.3,0.42,NA,0.21,4,1.08,19,7.2,3,4366.32664136963,147.385918503606,5131.81548598391,NA,19.1806971658852,39.4859307307951,387.304767920861,0.231415659389576,6.38908729652601,NA,4.97487373415292,7.70710678118655,1.56066017177982,7.30330085889911,1.56066017177982,0.0299575943120445,0.238034996345677,34.0710678118655,1.97769396754626,5.08400182501203,1.49746915806749,NA,NA,0.219981534000718,0.0576771815052812,NA,0.0968460667016911,0.398122915364962,0.104765493670665,3.02622826150877,0.799859093360379,0.35588780104607,66
"UOR150","UOR150","North America","Columbia Plateau","USA","Oregon","Glass Buttes","Glass Buttes Group General","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.54,-120.066,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","""Literature suggests alternate names for this source include: Glass Butte Crescent (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992). ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773. ; Nelson, Fred W, Jr. X-Ray Fluorescence Analysis of Some Western North American Obsidians. Obsidian Studies in the Great Basin (1984) 27-62. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28932.2362052275,542.724227763305,35530.0522315173,NA,719.278918377566,387.225464490118,1958.36934059741,0.3,20,NA,97,73,27,88,11,0.2,3.4,1370,27,49,18,NA,NA,3.7,0.54,NA,0.41,3.4,0.76,21,8.4,3.2,4589.93905696539,88.4315511021639,4455.20695334912,NA,13.5393156465072,32.9049422756625,301.237041716226,0.0771385531298588,2.9559739536744,NA,9.37756967007256,15.5978441670209,3.33611846334397,10.0542323528153,1.53446470463976,0.0149787971560223,0.289042495562608,151.078822757653,2.32164074451082,6.55568656383131,2.45040407683772,NA,NA,0.353883337305502,0.0741563762210758,NA,0.189080415941397,0.338404478060218,0.0737238659163942,3.34477860482548,0.933168942253775,0.379613654449141,2
"UUT008","UUT008","North America","Colorado Plateau Transition Zone","USA","Utah","Pumice Hole Mine","Pumice Hole Mine Group General","0.5-0.8","",0.65,"","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",38.411,-112.831,"","Mineral Mountain Range","","","Obsidian","""The Mineral Mountains composed of lava domes, flows, and tuffs from 500,000 to 800,000 years ago. The Mineral Mountains have three distinct rhyolite sequences, with obsidian being found in the lower two: known as the Wildhorse Canyon and Pumice Hole sources (Haarklau et al 2005).""","","""Literature suggests alternate names for this source include: Mineral Mountains, Mineral Mountain Range (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Nelson, Fred W, Jr. X-Ray Fluorescence Analysis of Some Western North American Obsidians. Obsidian Studies in the Great Basin (1984) 27-62. ; Unknown. Department of Development Services, Division of State History, 1979 - Indians of North America, Antiquities Section Selected Papers, Volume 6, Issues 14-15 (1979). ; Kaiser, Bruce Personal Communication 2017.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25519.7160374314,NA,38566.2,NA,986.011517275914,644.993766857443,5509.01232074645,NA,33.3,18.5,177.191666666667,41.1833333333333,20.9727272727273,122.258333333333,23.1545454545455,NA,NA,328,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.9,NA,4048.56162973357,NA,1667.67548135454,NA,12.7151750187325,1041.11701672689,279.467397929697,NA,2.62678510731274,0.52704627669473,7.9546965353618,11.4098707930963,1.76866667808884,14.7826961702054,0.991326017376359,NA,NA,36.1706962514672,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.10050493461461,NA,12
"UWA006","UWA006","North America","Cascadia","USA","Washington","Copper Mountain","Copper Ridge A","","",NA,"","Active","Convergent","Continental","Active Continental Margin",48.96,-121.408,"","","Garibaldi Volcanic Belt or Cascade Arc","","Obsidian","","","""Literature suggests alternate names for this source include: Copper Ridge #1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Mierendorf, Robert R. Archaeology of the Little Beaver Watershed North Cascades National Park Service Complex, Whatcom County, Washington. National Park Service, North Cascades National Park Service Complex, Sedro Woolley, Washington (2004).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,664.75,272.5,NA,NA,40.5,NA,95.75,74.5,22,187,13.75,NA,NA,746.5,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,22.25,NA,NA,NA,NA,NA,NA,148.627481359022,67.143441660804,NA,NA,5.64791576165636,NA,4.97311099736245,7.59267638593623,2.20710678118655,7.21931893407023,1.85867789130417,NA,NA,43.1259371274066,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,9.5749068152066,NA,NA,4
"UWA007","UWA007","North America","Cascadia","USA","Washington","Copper Mountain","Copper Ridge B","","",NA,"","Active","Convergent","Continental","Active Continental Margin",48.937,-121.444,"","","Garibaldi Volcanic Belt or Cascade Arc","","Obsidian","","","""Literature suggests alternate names for this source include: Copper Ridge #2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Mierendorf, Robert R. Archaeology of the Little Beaver Watershed North Cascades National Park Service Complex, Whatcom County, Washington. National Park Service, North Cascades National Park Service Complex, Sedro Woolley, Washington (2004).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,695.5,248.9,NA,NA,46.8,NA,132.8,101.9,14.7,116.6,10.7,NA,NA,717.5,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23.1,NA,NA,NA,NA,NA,NA,129.569812864567,51.6172643682766,NA,NA,22.2580983078352,NA,5.47871685541036,8.01202098103869,2.24721705904866,7.38873015549064,2.14206982955429,NA,NA,13.9675144212722,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.59241310156125,NA,NA,10
"UWA023","UWA023","North America","Cascadia","USA","Washington","Agnes Creek","Agnes Creek Group general","","",NA,"","Active","Convergent","Continental","Active Continental Margin",48.188,-120.961,"","","","Low","Obsidian","""Geochemical data provided for this sample came from a fine-ash rhyolite proxy of Phelps Creek, from the Glacier Peak eruption (Randle et al 1971).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Randle, Keith, Gordon G. Goles, and Laurence R. Kittleman. Geochemical and Petrological Characterization of Ash Samples from Cascade Range Volcanoes. Quaternary Research 1 (1971) 261-282.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,22900,9.8,NA,NA,23,NA,NA,NA,NA,NA,1.7,220,13.5,30.7,NA,NA,NA,2.56,0.82,1.02,0.2,3.13,NA,NA,5.58,NA,NA,NA,NA,0.14,NA,NA,200,0.2,NA,NA,4,NA,NA,NA,NA,NA,0.3,50,0.7,0.8,NA,NA,NA,0.15,0.03,0.08,0.03,0.09,NA,NA,0.13,NA,1
"UWY022","UWY022","North America","Yellowstone","USA","Wyoming","Teton Pass","Teton Pass Variety 1","","",NA,"","Hotspot","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",43.498,-110.95,"","Yellowstone Crescent of High Terrane","","","Obsidian","","","""Literature suggests alternate names for this source include: Fish Creek 1, Fish Creek Variety 1, Fish Creek/McNeely Ranch, Mosquito Creek, Phillips Ridge, Teton Pass Variety 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Frison, George C. and Danny N. Walker. Medicine Lodge Creek: Holocene Archaeology of the Eastern Big Horn Basin, Wyoming. Volume 1. Covis Press. 2007. ; Shackley, Steven M. Source Provenance of Obsidian Artifacts from a Number of Prehistoric Sites in Park County, Wyoming. Archaeological Research Facility, UC Berkeley (2011). ; Hughes, Richard E. Personal Communication, 2005. ; Black, Marielle Loryn Pedro. Using X-Ray Fluorescence Spectrometry to Assess Variance in Obsidian Source Distribution in Southern Idaho. Boise State University, 2014.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1060.16666666667,374.857142857143,2197.33333333333,NA,411,16,130.666666666667,116.555555555556,26.4444444444444,74.6666666666667,12.3333333333333,NA,NA,1362.33333333333,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,12,NA,NA,NA,NA,NA,172.116334804038,31.1499121529601,1397.0599575566,NA,41,0.4,17.8804990323406,18.2255711416765,3.05412013996749,3.98153744329409,2.151387818866,NA,NA,107.487915936544,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2,NA,9
"UWY023","UWY023","North America","Yellowstone","USA","Wyoming","Teton Pass","Teton Pass Variety 2","","",NA,"","Hotspot","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",43.498,-110.95,"","Yellowstone Crescent of High Terrane","","","Obsidian","","","""Literature suggests alternate names for this source include: Crescent H, Fish Creek 2, Fish Creek Variety 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Clayton, Carmen and Raymond Kunselman. Obsidian Source Utilization at the Trappers Point Antelope Kill Site 48SU1006. The Wyoming Archaeologist 46 (2002) 83-91. ; Kaiser, Bruce Personal Communication 2017.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,21426.25,NA,NA,286.75,10645,NA,47.25,17.75,112.933333333333,159,48.4666666666667,153.4,33.7333333333333,NA,NA,NA,NA,NA,NA,NA,NA,12,0.16,NA,68,NA,NA,NA,17.8,6.4,NA,NA,1511.05931385899,NA,NA,34.7023053989213,588.269212747588,NA,4.57347424467075,0.957427107756338,11.6463769146501,23.4459865587756,19.7117320637325,31.1374831536343,17.3100576324314,NA,NA,NA,NA,NA,NA,NA,NA,1.14772974261244,0.0219722596210595,NA,31.3596787415,NA,NA,NA,6.83373982530795,0.759227308898283,15
"RPN004","RPN004","Pacific","Pacific","Chile","Easter Island","Rano Kau","Rano Kau II","","0.3-0",0.15,"Shield","Active","Divergent","Oceanic","Extensional Zone in Oceanic Basin",-27.178,-109.417,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Te Manavai (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Leach, Foss. New Zealand and Oceanic Obsidians: An Archaeological Perspective Using Neutron Activation Analysis. Journal of the Royal Society of New Zealand 26, 1 (1996) 79-105. ; Bonatti, E., C. G. A. Harrison, D. E. Fisher, J. Honnorez, J.-G. Schilling, J. J. Stipp, and M. Zentilli. Easter Volcanic Chain (Southeast Pacific): A Mantle Hot Line. Journal of Geophysical Research 82, 17 (1977) 2457-2478.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,45000,NA,NA,NA,NA,NA,19000,0.1,NA,NA,80.2,NA,NA,7966,NA,0.3,1,509,104.6,181.1,110.5,NA,NA,27.3,4.2,34.8,1.9,22.9,8.8,NA,9.4,2.6,8000,NA,NA,0.1,NA,NA,4000,0.1,NA,NA,17.9,NA,NA,100.1,NA,0.1,0.1,106,19,24.2292823818337,19.1,NA,NA,5.8,0.9,6.3,0.4,3.5,1.5,NA,1,0.4,4
"RPN005","RPN005","Pacific","Pacific","Chile","Easter Island","Rano Kau","Rano Kau Group General","","0.3-0",0.15,"Shield","Active","Divergent","Oceanic","Extensional Zone in Oceanic Basin",-27.178,-109.417,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Leach, Foss. New Zealand and Oceanic Obsidians: An Archaeological Perspective Using Neutron Activation Analysis. Journal of the Royal Society of New Zealand 26, 1 (1996) 79-105. ; Smith, I. E. M., G. K. Ward, and W. R. Ambrose. Geographic Distribution and the Characterization of Volcanic Glasses in Oceania. Archaeology and Physical Anthropology in Oceania 12, 3 (1977) 173-201. ; Bonatti, E., C. G. A. Harrison, D. E. Fisher, J. Honnorez, J.-G. Schilling, J. J. Stipp, and M. Zentilli. Easter Volcanic Chain (Southeast Pacific): A Mantle Hot Line. Journal of Geophysical Research 82, 17 (1977) 2457-2478.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,42000,NA,NA,NA,NA,NA,48000,0.1,NA,NA,79.4666666666667,25,137.5,867.266666666667,112.5,0.3,1,466,1057,185.01,109.1,NA,NA,26.2,3.5,34.1,1.8,21.6,8.5,9.5,10.3,30,6663.06741812495,NA,NA,NA,NA,NA,7383.37641558867,0.0257128510432863,NA,NA,0.503322295684716,5.34172745445921,0.707106781186548,108.125914254324,0.707106781186548,0.0224681957340334,0.0850124986948847,51.3888550401943,90.8879358128866,24.7523994117231,14.8521713768331,NA,NA,2.50587660470383,0.7,6.2,0.3,3.7,1.6,2.12132034355964,2,3.5588780104607,3
"JVA001","JVA001","Pacific","Southeast Asia","Indonesia","West Java","Nagrek","Nagrek A","","33.9-23",28.45,"","Active","Subduction","Continental","Mature Island Arc",-6.734,108.007,"","","Silicic and Intermediate Volcanism from Oceanic Subduction over Old and Thick Continental Crust","","Obsidian","","","""Literature suggests alternate names for this source include: Leles (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Neri, Leee Anthony N., Alfred F. Pawlik, Christian Reepmeyer, Armand Salvador B. Mijares, and Victor J. Paz. Mobility of Early Islanders in the Philippines During the Terminal Pleistocene/Early Holocene Boundary: pXRF-Analysis of Obsidian Artefacts. Journal of Archaeological Science 61 (2010) 149-157. ; Reepmeyer, Christian, Matthew Spriggs, Anggraeni, Peter Lape, Leee Neri, Wilfredo P. Ronquillo, Truman Simanjuntak, Glenn Summerhayes, Daud Tanudirjo, and Archie Tiauzon. Obsidian Sources and Distribution Systems in Island Southeast Asia: New Results and Implications from Geochemical Research using LA-ICPMs. Journal of Archaeological Science 38 (2011) 2995-3005. ; Katili, John A. Volcanism and Plate Tectonics in the Indonesian Island Arcs. Tectonophysics 26 (1975) 165-188.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,765.4,234.05,NA,NA,NA,NA,187.2,29.6,37.6,96.4,7.5,NA,NA,316,0.3,0.8,NA,NA,NA,NA,0.01,NA,NA,NA,NA,NA,10.95,0.1,NA,NA,NA,NA,9.7,2.93535533905933,NA,NA,NA,NA,2.70000000000002,0.300000000000002,0.4,0.55000000000001,0.1,NA,NA,5.4,23.8,0.107031617368674,NA,NA,NA,NA,0.46,NA,NA,NA,NA,NA,12.4306872196367,0.0118629267015357,12
"JVA002","JVA002","Pacific","Southeast Asia","Indonesia","West Java","Nagrek","Nagrek B","","33.9-23",28.45,"","Active","Subduction","Continental","Mature Island Arc",-6.734,108.007,"","","Silicic and Intermediate Volcanism from Oceanic Subduction over Old and Thick Continental Crust","","Obsidian","","","""Literature suggests alternate names for this source include: Leles (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Neri, Leee Anthony N., Alfred F. Pawlik, Christian Reepmeyer, Armand Salvador B. Mijares, and Victor J. Paz. Mobility of Early Islanders in the Philippines During the Terminal Pleistocene/Early Holocene Boundary: pXRF-Analysis of Obsidian Artefacts. Journal of Archaeological Science 61 (2010) 149-157. ; Reepmeyer, Christian, Matthew Spriggs, Anggraeni, Peter Lape, Leee Neri, Wilfredo P. Ronquillo, Truman Simanjuntak, Glenn Summerhayes, Daud Tanudirjo, and Archie Tiauzon. Obsidian Sources and Distribution Systems in Island Southeast Asia: New Results and Implications from Geochemical Research using LA-ICPMs. Journal of Archaeological Science 38 (2011) 2995-3005. ; Katili, John A. Volcanism and Plate Tectonics in the Indonesian Island Arcs. Tectonophysics 26 (1975) 165-188.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1206.3,233.45,NA,NA,NA,NA,170.6,46.9,31.9,141.7,7.1,NA,NA,397.2,24.7,49.6,NA,NA,NA,NA,0.45,NA,NA,NA,NA,NA,17.2,3.3,NA,NA,NA,NA,22.7067359366264,0.636396103067897,NA,NA,NA,NA,16.4929215022101,10.0210807045655,3.94156218446935,16.18959914084,0.990427218449302,NA,NA,43.8018309484231,2.1238713477562,6.63596027685781,NA,NA,NA,NA,0.0617969801842298,NA,NA,NA,NA,NA,2.9698484809835,0.391476581150677,2
"JVA003","JVA003","Pacific","Southeast Asia","Indonesia","West Java","Nagrek","Nagrek Group General","","33.9-23",28.45,"","Active","Subduction","Continental","Mature Island Arc",-6.734,108.007,"","","Silicic and Intermediate Volcanism from Oceanic Subduction over Old and Thick Continental Crust","","Obsidian","","","""Literature suggests alternate names for this source include: Leles (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Smith, I. E. M., G. K. Ward, and W. R. Ambrose. Geographic Distribution and the Characterization of Volcanic Glasses in Oceania. Archaeology and Physical Anthropology in Oceania 12, 3 (1977) 173-201. ; Neri, Leee Anthony N., Alfred F. Pawlik, Christian Reepmeyer, Armand Salvador B. Mijares, and Victor J. Paz. Mobility of Early Islanders in the Philippines During the Terminal Pleistocene/Early Holocene Boundary: pXRF-Analysis of Obsidian Artefacts. Journal of Archaeological Science 61 (2010) 149-157. ; Katili, John A. Volcanism and Plate Tectonics in the Indonesian Island Arcs. Tectonophysics 26 (1975) 165-188. ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24942.4745309547,1959.83748914527,38041.2299885345,NA,644.35403104657,348.502918041106,5712.91653615835,NA,NA,NA,193,28,NA,126.5,7.5,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19,NA,6,987.400604144345,1993.03209862462,3501.30447571591,NA,57.3880945410282,54.7619503578142,4174.24474305245,NA,NA,NA,1.4142135623731,5.98273474899432,NA,0.707106781186548,0.707106781186548,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.02622826150877,NA,0.71177560209214,9
"MAL004","MAL004","Pacific","Southeast Asia","Indonesia","Maluku","Mount Rano","Mount Rano SW","","",NA,"","","","","Mature Island Arc",1.26805555,124.8783333,"","","","","Obsidian","","","",""" ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34904.1464988706,1386.96191539511,28224.8078474669,NA,1738.25738607912,774.450928980236,3671.94251362014,1.1,56.5,NA,75,122.5,55,239,6,NA,4.9,527.5,20.5,46,26.5,NA,NA,6.85,1.135,NA,0.815,6.85,0.375,19,5.85,1.55,786.853092907923,170.561769673627,939.197789488524,NA,254.303500374649,65.8098845513251,346.194060201062,0.141421356237309,7.77817459305202,NA,1.4142135623731,24.7487373415292,4.24264068711928,5.65685424949238,0.836980747985326,NA,0.282842712474619,3.53553390593274,0.707106781186548,1.4142135623731,3.53553390593274,NA,NA,0.0707106781186551,0.0919238815542511,NA,0.0353553390593273,0.0707106781186551,0.0494974746830583,1.4142135623731,0.494974746830583,0.212132034355964,4
"MAL005","MAL005","Pacific","Southeast Asia","Indonesia","Maluku","Mount Rano","Mount Rano W","","",NA,"","","","","Mature Island Arc",1.251388889,127.433333,"","","","","Obsidian","","","",""" ; Macdonald, R, R. L. Smith, and J. E. Thomas. Chemistry of Subalkalic Silicic Obsidians. U.S. Geological Survey Professional Paper 1523 (1992).""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,34125.2016779606,1507.56729934251,27726.7230030999,NA,1858.13720580871,774.450928980236,4126.56396768739,1.2,53,NA,76,133,49,242,4.5,NA,4.5,550,20,45,27,NA,NA,6.6,1.14,NA,0.79,6.6,0.28,28,5.5,1.6,5413.77427231814,245.64319750601,3476.72692153879,NA,34.9765654201436,65.8098845513251,634.749480759189,0.308554212519435,7.83333097723715,NA,7.34737417448984,28.417990057723,6.05443721125386,27.649138970242,0.627735560988995,NA,0.382556244126981,60.6520821289847,1.71973388482283,6.02052847698793,3.67560611525658,NA,NA,0.631251358436842,0.156552349800049,NA,0.364325679496838,0.656902810352187,0.0271614242849873,4.45970480643397,0.611003474094734,0.189806827224571,2
"PNG010","PNG010","Pacific","Southeast Asia","Papua New Guinea","West New Britain","Garala","Garala Group","","2.6-0",1.3,"Shield","Active","Subduction","Oceanic","Mature Island Arc",-9.535,150.698,"LOCATION IS UNKNOWN AND APPROXIMATED"," Willaumez Peninsula","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Sheppard, Peter, Barbara Trichereau, and Cristany Milicich. Pacific Obsidian Sourcing by Portable XRF. Archaeology Oceania 45 (2010) 21-30. ; McInnes, Brent I. A., and Eion M. Cameron. Carbonated, Alkaline Hybridizing Melts from a Sub-Arc Environment: Mantle Wedge Samples from the Tabar-Lihir-Tanga-Feni Arc, Papua New Guinea. Earth and Planetary Science Letters 122 (1994) 125-141. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,46716.21,NA,1572.46,525.87,11123.41,NA,47.04,NA,59.86,143.06,NA,159.24,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10.4,NA,NA,NA,NA,6834.46,NA,76.41,41.95,632.04,NA,5.86,NA,6.74,19.96,NA,11.29,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.19,NA,NA,16
"PNG049","PNG049","Pacific","Southeast Asia","Papua New Guinea","Admiralty Islands","Pam Islands","Pam Mandian","","",NA,"","","","Oceanic","Primitive Island Arc",-2.505,147.331,"","St Andrews Strait","","","Obsidian","","","""Literature suggests alternate names for this source include: Mandian (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Torrence, Robin, Sarah Kelloway, and Peter White. Stemmed Tools, Social Interaction, and Voyaging in Early-Mid Holocene Papua New Guinea. Journal of Island and Coastal Archaeology 8 (2013) 278-310. ; Summerhayes, Glenn R., Jean Kennedy, Elizabeth Matisoo-Smith, Herman Mandui, Wal Ambrose, Charolette Allen, Christan Reepmeyer, Robin Torrence, and François Wadra. Lepong: A New Obsidian Source in the Admiralty Islands, Papua New Guinea. Geoarchaeology: An International Journal 0 (2014) 1-11.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,571,16764,NA,43,14,155,54,46,320,45,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7,NA,NA,NA,NA,NA,NA,45,1681,NA,5,1,5,5,3,21,3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1,NA,4
"PNG050","PNG050","Pacific","Southeast Asia","Papua New Guinea","Admiralty Islands","Pam Islands","Pam Islands Group General","","",NA,"","","","Oceanic","Primitive Island Arc",-2.495,147.339,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Sheppard, Peter, Barbara Trichereau, and Cristany Milicich. Pacific Obsidian Sourcing by Portable XRF. Archaeology Oceania 45 (2010) 21-30. ; Torrence, Robin, Sarah Kelloway, and Peter White. Stemmed Tools, Social Interaction, and Voyaging in Early-Mid Holocene Papua New Guinea. Journal of Island and Coastal Archaeology 8 (2013) 278-310. ; Bird, J. R., L. H. Russell, M. D. Scott, and W. R. Ambrose. Obsidian Characterisation with Elemental Analysis by Proton Induced Gamma-Ray Emission. Analytical Chemistry 50, 14 (1978) 2082-2084.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33700,NA,46272.16,NA,1661.54,556.016923076923,15719.4507692308,NA,43.7661538461538,14,156.092307692308,48.3369230769231,44,308.824615384615,43,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,7.56,7,NA,600,NA,1401.19,NA,12.44,39.375885437885,826.92412192124,NA,5.20838819284681,1,4.59136280358673,4.21227665191855,3,27.5497301372703,3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2.38,1,NA,21
"PNG051","PNG051","Pacific","Southeast Asia","Papua New Guinea","West New Britain","Garala","Garala B","","2.6-0",1.3,"Shield","Active","Subduction","Oceanic","Mature Island Arc",-5.293,150.093,""," Willaumez Peninsula","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Sheppard, Peter, Barbara Trichereau, and Cristany Milicich. Pacific Obsidian Sourcing by Portable XRF. Archaeology Oceania 45 (2010) 21-30. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,21400,NA,47500,NA,1560,504,11900,NA,NA,NA,57,146,29,172,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1800,NA,3900,NA,100,31,600,NA,NA,NA,4,31.1956883340418,3,10,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10
"PNG052","PNG052","Pacific","Southeast Asia","Papua New Guinea","West New Britain","Garala","Garala C","","2.6-0",1.3,"Shield","Active","Subduction","Oceanic","Mature Island Arc",-5.293,150.093,""," Willaumez Peninsula","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Sheppard, Peter, Barbara Trichereau, and Cristany Milicich. Pacific Obsidian Sourcing by Portable XRF. Archaeology Oceania 45 (2010) 21-30. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,25600,NA,33600,NA,1390,455,10700,NA,NA,NA,55,129,26,153,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1600,NA,3500,NA,80,31,600,NA,NA,NA,5,13,3,16,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10
"ARG005","ARG005","South America","Andes South","Argentina","Neuquen","Cerro Bayo","Cerro Bayo 1","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-38.772,-70.705,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stern, C. R., I. Pereda, and A. M. Aguerre. Multiple Primary and Secondary Sources for Chemically Similar Obsidians from the Area of Portada Covunco, West-Central Neuquen, Argentina. Archaeometry 54, 3 (2012) 442-453.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1219,509,NA,NA,NA,NA,160,52,19,181,30,NA,NA,284,31.4,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,20.5,22.7,6.7,NA,NA,NA,NA,22.9457938379736,43.2528775977223,NA,NA,NA,NA,15.4681561568207,11.1107931052752,2.34763891864946,20.679727907495,4.18490373992663,NA,NA,31.3185296811485,2.69998219917184,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.2651410189963,2.52177797490008,0.79481608900289,4
"ARG006","ARG006","South America","Andes South","Argentina","Neuquen","Cerro Bayo","Cerro Bayo 2","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-38.772,-70.705,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Stern, C. R., I. Pereda, and A. M. Aguerre. Multiple Primary and Secondary Sources for Chemically Similar Obsidians from the Area of Portada Covunco, West-Central Neuquen, Argentina. Archaeometry 54, 3 (2012) 442-453.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1232,427,NA,NA,NA,NA,191,9,18,151,32,NA,NA,NA,33.7,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,23.7,26.6,7.5,NA,NA,NA,NA,23.1904987763605,36.2848305191108,NA,NA,NA,NA,18.4651114122047,1.92302188360532,2.22407897556264,17.252148696308,4.46389732258841,NA,NA,NA,2.89775159592647,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,3.77482156830304,2.95503498380362,0.889719502615175,2
"ARG012","ARG012","South America","Andes South","Argentina","Mendoza","El Peceño","El Peceño-1","","32-10",21,"Cone","","","Continental","Active Continental Margin",-35.292624,-68.6311769,"","","Northern Patagonia","","Obsidian","""The obsidian source known as Cerro el Peceño is from El Nevada Volcano, a relatively small cone with many alluvial deposits. Nodules from this source vary in size, up to 30cm across (Duran et al 2011). Being on the Eastern Plains of Southern Mendoza, this source was easily accesible and has been exploited historically. Samples from El Peceño are more likely to be found in the alluvial deposits than El Peceño-1 (Salgán and Pompeo 2017).""","","""Literature suggests alternate names for this source include: Cerro el Peceño 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Giesso, M., V. Durán, G. Neme, M.D. Glascock, V. Cortegoso, A. Gil, and L. Sanhueza. A Study of Obsidian Source Usage in the Central Andes of Argentina and Chile. Archaeometry 53, 1 (2011) 1-21. ; Jordan, Teresa E., W. Matthew Burns, Ricardo Veiga, Francisco Pangaro, Peter Copeland, Shari Kelley, and Constantino Mpodozis. Extension and Basin Formation in the Southern Andes Caused by Increased Convergent Rate: A Mid-Cenozoic Trigger for the Andes. Tectonics 20, 3 (2001) 308-324. ; Salgán, M. Laura and M. Paz Pompei. Fuente e Obsidiana El Peceño: Primeros Resultados de au Abordaje Tecnológico, Ggeoquímico y Espacial. Revista del Museo de Antropología, Suplemento Especial 1 (2017) 51-58.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33400,NA,34138.5964912281,NA,1720,768.578947368421,5966.73684210526,NA,44.4210526315789,NA,222.070175438596,370.105263157895,18,169.122807017544,22,0.49,NA,1127,18.4,34.2,NA,NA,1.09,2.48,0.47,NA,NA,NA,NA,NA,11.4,8.15,800,NA,3628.38250608274,NA,131,93.7966135925585,239.814009338127,NA,6.72408577849736,NA,5.84597098439531,21.3654477046631,2,22.2291115849845,2,0.0366980530322545,NA,20,0.9,1.6,NA,NA,0.24,0.2,0.0645435126368623,NA,NA,NA,NA,NA,0.3,0.45,57
"ARG013","ARG013","South America","Andes South","Argentina","Mendoza","El Peceño","El Peceño-2","","32-10",21,"Cone","","","Continental","Active Continental Margin",-35.29686,-68.628747,"","","Northern Patagonia","","Obsidian","""The obsidian source known as Cerro el Peceño is from El Nevada Volcano, a relatively small cone with many alluvial deposits. Nodules from this source vary in size, up to 30cm across (Duran et al 2011). Being on the Eastern Plains of Southern Mendoza, this source was easily accesible and has been exploited historically. Samples from El Peceño are more likely to be found in the alluvial deposits than El Peceño-1 (Salgán and Pompeo 2017).""","","""Literature suggests alternate names for this source include: Cerro el Peceño 2 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Giesso, M., V. Durán, G. Neme, M.D. Glascock, V. Cortegoso, A. Gil, and L. Sanhueza. A Study of Obsidian Source Usage in the Central Andes of Argentina and Chile. Archaeometry 53, 1 (2011) 1-21. ; Jordan, Teresa E., W. Matthew Burns, Ricardo Veiga, Francisco Pangaro, Peter Copeland, Shari Kelley, and Constantino Mpodozis. Extension and Basin Formation in the Southern Andes Caused by Increased Convergent Rate: A Mid-Cenozoic Trigger for the Andes. Tectonics 20, 3 (2001) 308-324. ; Salgán, M. Laura and M. Paz Pompei. Fuente e Obsidiana El Peceño: Primeros Resultados de au Abordaje Tecnológico, Ggeoquímico y Espacial. Revista del Museo de Antropología, Suplemento Especial 1 (2017) 51-58.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31100,NA,32970.5882352941,NA,1308,620.176470588235,5047.64705882353,NA,42.7058823529412,NA,243.352941176471,369.588235294118,16,112.411764705882,20,0.7,NA,866,7.8,15.7,NA,NA,0.62,1.62,0.23,NA,NA,NA,NA,NA,9.37,9.6,1000,NA,4099.50513133846,NA,192,114.697183921139,263.940972576052,NA,7.01292281535206,NA,5.73957961650586,48.4950768002015,1,20.1715473884368,1,0.11,NA,14,0.1,0.2,NA,NA,0.1,0.07,0.01,NA,NA,NA,NA,NA,0.2,0.2,17
"ARG018","ARG018","South America","Andes South","Argentina","Mendoza","Laguna del Diamante","Laguna del Diamante Arroyo las Numeradas subsource","","32-10",21,"Caldera","","","Continental","Active Continental Margin",-34.157,-69.823,"","","Region of ""Active Margin"" Basins","","Obsidian","""Laguna del Diamante obsidian is found in the Cordillera Principal Volcanic Complex, near the a lagoon and river of the same name. There are two subsources: Arroyo las Numeradas and Arroyo Paramillos. Arroyo Las Numerals is widely distributed within the caldera along the crests and ridges, as well as the surrounding valleys (Duran et al 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Durán, Víctor, Anna Maria De Francisco, Valeria Cortegoso, Gustavo Neme, Luis Cornejo, and Marco Bocci. (2011) Caracterización y Procedencia de Obsidianas de Sitios Arqueológicos del Central Oeste de Argentina y Centro Chile con Metodología no Destructiva por Fluorescencia de Rayos X (XRF). Intersecciones en Antropología 13 (2012) 423-437. ; Jordan, Teresa E., W. Matthew Burns, Ricardo Veiga, Francisco Pangaro, Peter Copeland, Shari Kelley, and Constantino Mpodozis. Extension and Basin Formation in the Southern Andes Caused by Increased Convergent Rate: A Mid-Cenozoic Trigger for the Andes. Tectonics 20, 3 (2001) 308-324.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1111,473.5,65,583,161,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,217.788888605457,127.986327394765,11.3137084989848,115.965512114594,91.9238815542512,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,2
"ARG019","ARG019","South America","Andes South","Argentina","Mendoza","Laguna del Diamante","Laguna del Diamante Arroyo Paramillos subsource","","32-10",21,"","","","Continental","Active Continental Margin",-34.157,-69.823,"","","Region of ""Active Margin"" Basins","","Obsidian","""Laguna del Diamante obsidian is found in the Cordillera Principal Volcanic Complex, near the a lagoon and river of the same name. There are two subsources: Arroyo las Numeradas and Arroyo Paramillos. Arroyo Paramillos obsidian can be found only in the glacial and alluvial deposits near the caldera. Typically, Arroyo Paramillos nodules are less than 3 cm across (Duran et al 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Durán, Víctor, Anna Maria De Francisco, Valeria Cortegoso, Gustavo Neme, Luis Cornejo, and Marco Bocci. (2011) Caracterización y Procedencia de Obsidianas de Sitios Arqueológicos del Central Oeste de Argentina y Centro Chile con Metodología no Destructiva por Fluorescencia de Rayos X (XRF). Intersecciones en Antropología 13 (2012) 423-437. ; Jordan, Teresa E., W. Matthew Burns, Ricardo Veiga, Francisco Pangaro, Peter Copeland, Shari Kelley, and Constantino Mpodozis. Extension and Basin Formation in the Southern Andes Caused by Increased Convergent Rate: A Mid-Cenozoic Trigger for the Andes. Tectonics 20, 3 (2001) 308-324.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1028.5,570.3,59.1,746,186.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,307.427407872348,388.827882516445,27.0737675414577,680.628304501722,206.76245092161,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10
"ARG025","ARG025","South America","Patagonia","Argentina","Santa Cruz","Pampa del Asador","Pampa del Asador 1","4.9-6.4","",5.65,"","","","Continental","Active Continental Margin",-47.994,-71.178,"","","Southern Patagonia","High","Obsidian","""Pampa del Asador obsidian is found primarily in fluvial and glacial secondary deposits in the Santa Cruz Province of Argentina. Nodules are translucent grey to black, up to 20 cm across, and may contain a brown-grey tint in more weathered samples. Pampa del Asador varieties 1 and 2 are free of phenocrysts, while a third variety contains small plagioclase feldspar inclusions (Fernandez et al 2015).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Fernández, María Victoria, Charles R. Stern, and Pablo Rodrigo Leal. Geochemical Analysis of Obsidian from Archaeological Sites in Northwest Santa Cruz Province, Argentine Patagonia. Quaternary International 375 (2015) 44-54. ; Nami, Hugo G., Martin Giesso, Alicia Castro, and Michael D. Glascock. New Analyses of Late Holocene Obsidians from Southern Patagonia (Santa Cruz Province, Argentina). International Association for Obsidian Studies 57 (2017) 13-25.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,37121,NA,772.775510204082,294.65306122449,10295.2727272727,NA,85.5454545454545,19.9090909090909,192.408163265306,32.8163265306122,31.734693877551,128.571428571429,25.6530612244898,NA,NA,232,37,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,18.0204081632653,5.6,NA,NA,1142.6351123609,NA,68.0267092357115,51.7858269905216,528.202061887133,NA,14.2503588471564,1.81408629643385,14.2156151030272,2.09944248797069,2.43317245854497,7.89776204506436,3.12133829737819,NA,NA,10,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.54639780980285,0.3,49
"ARG026","ARG026","South America","Patagonia","Argentina","Santa Cruz","Pampa del Asador","Pampa del Asador 2","4.9-6.4","",5.65,"","","","Continental","Active Continental Margin",-47.994,-71.178,"","","Southern Patagonia","High","Obsidian","""Pampa del Asador obsidian is found primarily in fluvial and glacial secondary deposits in the Santa Cruz Province of Argentina. Nodules are translucent grey to black, up to 20 cm across, and may contain a brown-grey tint in more weathered samples. Pampa del Asador varieties 1 and 2 are free of phenocrysts, while a third variety contains small plagioclase feldspar inclusions (Fernandez et al 2015).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Fernández, María Victoria, Charles R. Stern, and Pablo Rodrigo Leal. Geochemical Analysis of Obsidian from Archaeological Sites in Northwest Santa Cruz Province, Argentine Patagonia. Quaternary International 375 (2015) 44-54. ; Nami, Hugo G., Martin Giesso, Alicia Castro, and Michael D. Glascock. New Analyses of Late Holocene Obsidians from Southern Patagonia (Santa Cruz Province, Argentina). International Association for Obsidian Studies 57 (2017) 13-25.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,36544.6666666667,NA,692.9375,289,9929,NA,92.8888888888889,20.7777777777778,219.5625,2.625,42.125,145.9375,30.375,NA,NA,28,26,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,18.675,6.2,NA,NA,1226.61709591869,NA,66.150175364474,59.5457088867956,1187.91392785841,NA,15.0286762927116,3.1135902820449,15.6796542846688,1.55798923145842,3.28518029533957,7.10771750501923,3.1525115306507,NA,NA,4,2,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.65078692034985,0.4,16
"ARG027","ARG027","South America","Patagonia","Argentina","Santa Cruz","Pampa del Asador","Pampa del Asador 3","4.9-6.4","",5.65,"","","","Continental","Active Continental Margin",-47.994,-71.178,"","","Southern Patagonia","","Obsidian","""Pampa del Asador obsidian is found primarily in fluvial and glacial secondary deposits in the Santa Cruz Province of Argentina. Nodules are translucent grey to black, up to 20 cm across, and may contain a brown-grey tint in more weathered samples. Pampa del Asador varieties 1 and 2 are free of phenocrysts, while a third variety contains small plagioclase feldspar inclusions (Fernandez et al 2015).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Fernández, María Victoria, Charles R. Stern, and Pablo Rodrigo Leal. Geochemical Analysis of Obsidian from Archaeological Sites in Northwest Santa Cruz Province, Argentine Patagonia. Quaternary International 375 (2015) 44-54. ; Nami, Hugo G., Martin Giesso, Alicia Castro, and Michael D. Glascock. New Analyses of Late Holocene Obsidians from Southern Patagonia (Santa Cruz Province, Argentina). International Association for Obsidian Studies 57 (2017) 13-25.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,35868.2857142857,NA,895.111111111111,438.666666666667,13982.1428571429,NA,73.1428571428571,19.7142857142857,180.666666666667,60.2222222222222,29.3333333333333,276.222222222222,30.8888888888889,NA,NA,520,41,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,19.5333333333333,6,NA,NA,657.503793217376,NA,170.715862926799,41.9073934171799,651.383509301914,NA,18.0686521488513,2.1380899352994,8.87002068626192,4.09957980596762,2.08339598873524,13.5561739004,1.31940745141143,NA,NA,20,1.6,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,1.2363184629246,0.71177560209214,9
"ARG047","ARG047","South America","Patagonia","Argentina","Chubut","Somuncura Plateau Group General","Somuncura","Mio","",14.25,"","Active","Convergent","Continental","Active Continental Margin",-42.136,-68.286,"LOCATION IS UNKNOWN AND APPROXIMATED","","","","Obsidian","","","","""Stern, Charles R. Obsidian Sources and Distribution in Patagonia, Southernmost South America. Quaternary International xxx (2017) 1-16.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,35386.3504356244,241.210767894802,36692.2502017071,NA,1012,957,3287.26282171708,NA,NA,NA,352,NA,56,456,164,NA,8.4,5,52.9,103,38.1,1.49,10.1,8.09,0.3,6.35,0.98,17.2,NA,NA,42.5,16.5,5613.84853890382,39.3029116009617,4600.93802191661,NA,19.0493382805819,81.3222079784288,505.647891452237,NA,NA,NA,34.0299435450056,NA,6.91935681286156,52.0992040100427,22.8774737782656,NA,0.714104989037032,0.551382564808952,4.54869612535639,13.7803207362168,5.1866886293065,0.201008121404199,1.02461852654894,0.773761134811219,0.0411979867894866,0.620220874458331,0.451948311274558,1.71192853606934,NA,NA,4.72139048164113,1.95738290575339,1
"CHL012","CHL012","South America","Andes South","Chile","Santiago Metropolitan","Laguna del Maule","Laguna del Maule Group General","","32-10",21,"","Active","Convergent","Continental","Active Continental Margin",-36.044,-70.524,"","","Region of ""Active Margin"" Basins","","Obsidian","""Obsidian from Laguna del Maule comes from the border of Argentina and Chile, as part of the Cordillera Principal Volcanic Complex. Nodules range from 3-5 cm and are heterogenous in composition (Duran et al 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Durán, Víctor, Anna Maria De Francisco, Valeria Cortegoso, Gustavo Neme, Luis Cornejo, and Marco Bocci. (2011) Caracterización y Procedencia de Obsidianas de Sitios Arqueológicos del Central Oeste de Argentina y Centro Chile con Metodología no Destructiva por Fluorescencia de Rayos X (XRF). Intersecciones en Antropología 13 (2012) 423-437. ; Giesso, Martín, Mónica A. Berón, and Michael D. Glascock. Obsidian in Western Pampas, Argentina: Source Characterization and Provisioning Strategies. International Association for Obsidian Studies 38 (2008) 15-18. ; Seelenfreund, Andrea, Javier Miranda, María Inés Dinator, and J. Roberto Morales. Caracterización de Obsidianas del Norte y Centro Sur de Chile Mediante Análisis de Fluorescencia de Rayos X. Chungara, Revista de Antropología Chilena 37, 2 (2005) 245-253. ; Jordan, Teresa E., W. Matthew Burns, Ricardo Veiga, Francisco Pangaro, Peter Copeland, Shari Kelley, and Constantino Mpodozis. Extension and Basin Formation in the Southern Andes Caused by Increased Convergent Rate: A Mid-Cenozoic Trigger for the Andes. Tectonics 20, 3 (2001) 308-324.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31854.5,NA,39757,NA,NA,449.75,73700,NA,28,NA,623.733333333333,350.333333333333,50.0909090909091,839.266666666667,78.6,NA,NA,643.8,33.25,61,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,24.25,6.125,5176.36201078196,NA,2451.27517835106,NA,NA,4.3493294502333,17000,NA,1.4142135623731,NA,195.891577548217,135.085485424025,33.1260974724199,310.163439707192,27.0932545930614,NA,NA,28.3776955085673,0.5,1.4142135623731,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.5,0.25,15
"ECU021","ECU021","South America","Andes North","Ecuador","Pichincha","Callejones","Callejones Group General","0.22-0.01","",0.115,"","","","Continental","Active Continental Margin",-0.223,-78.46,"","Sierra de Guamani","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Belot-Gurlet, Ludoviv, Olivier Dorighel, and Gérard Poupeau. Obsidian Provenance Studies in Colombia and Ecuador: Obsidian Sources Revisited. Journal of Archaeological Science 35 (2008) 272-289. ; Bigazzi, G., M. Coltelli, N. J. C. Hadler, A. M. Osorio Araya, M. Oddone, and E. Salazar. Obsidian-Bearing Lava Flows and Pre-Columbian Artifacts from the Ecuadorian Andes: First New Multidisciplinary Data. Journal of South American Earth Sciences 6, 2 (1992) 21-32. ; Knight, Charles L. F., Andrea M. Cuellar, Michael D. Glascock, Minard L. Hall, and Patricia A. Mothes. Obsidian Source Characterization in the Cordillera Real and Eastern Piedmont of the North Ecuadorian Andes. Journal of Archaeological Science 38 (2011) 1069-1079.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,10670,NA,NA,NA,126,130.375,9.75,156.5,12.375,NA,NA,1043.3,30.437,53.965,NA,NA,NA,NA,NA,NA,NA,NA,NA,22.5714285714286,17.678,7.042,NA,NA,NA,NA,NA,NA,876.812408671319,NA,NA,NA,12.5820860308968,7.00892288443809,1.16496474502143,48.6809339817277,1.06066017177982,NA,NA,138.628239867961,3.62912921909497,6.04576297914498,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.786795792469443,1.28489342402828,0.599199465954368,10
"ECU022","ECU022","South America","Andes North","Ecuador","Napo","Consanga","Cosanga Group General","0.54-0.0006","",0.2703,"","","","Continental","Active Continental Margin",-1.052,-77.825,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Pumayacu, Río Consanga (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Belot-Gurlet, Ludoviv, Olivier Dorighel, and Gérard Poupeau. Obsidian Provenance Studies in Colombia and Ecuador: Obsidian Sources Revisited. Journal of Archaeological Science 35 (2008) 272-289.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,136.06,159.14,15.972,81.8,20.508,NA,NA,1228.4,18.484,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,28.734,12.418,5.592,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,5.49709013933736,41.4994337310764,0.449521968317456,10.7480230740355,1.23586811594118,NA,NA,228.633549594105,6.17005915692872,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,0.333511618988004,1.95825687794017,0.227420315715198,5
"PER003","PER003","South America","Andes Central","Peru","Arequipa","Alca","Alca-1","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-15.12,-72.69,"","","","","Obsidian","""Alca-1 obsidian was heavily used in the Department of Cuzco, and is seldom found outside of it. Its location is still unknown but assumed to be in the Southern Highlands, and it was (probably) used during the Preceramic (Asaro and Burger 1997).""","","""Literature suggests alternate names for this source include: Cuzco Type (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Robert J. Speakman, and Richard L. Burger. Sources of Archaeological Obsidian in Peru: Description and Geochemistry. American Chemical Society Symposium Series: Chapter 28, (2007) 522-552. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,31600,NA,36850,NA,786,469.625,5522.125,NA,44,16,143.625,97.375,15,108.125,14,0.17,2.9,1013,29.12,57.96,NA,NA,1.982,3.3,0.492,1.09,NA,3.56,0.9,NA,14.124,3.326,600,NA,560.355339059327,0.023,17,11.7672215896712,115.901936554142,NA,2.20710678118655,1,8.87163274595973,18.1052954017325,1,7.27255123983,1,0.05,0.13,28.0099025766973,0.542842712474619,1.04819805153395,NA,NA,0.182961940777126,0.315625679218421,0.00676776695296637,0.04,NA,0.14,0.01,NA,0.45876659402887,0.147568542494924,132
"PER004","PER004","South America","Andes Central","Peru","Arequipa","Alca","Alca-2","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-15.12,-72.69,"","","","","Obsidian","""Alca-1 obsidian was heavily used in the Department of Cuzco, and is seldom found outside of it. Its location is still unknown but assumed to be in the Southern Highlands, and it was (probably) used during the Preceramic (Asaro and Burger 1997).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Robert J. Speakman, and Richard L. Burger. Sources of Archaeological Obsidian in Peru: Description and Geochemistry. American Chemical Society Symposium Series: Chapter 28, (2007) 522-552. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33400,NA,34200,NA,1062,473,7213.5,NA,50,13,142.5,185.5,15,150.5,8,NA,NA,952,43.5,80,NA,NA,1.8,NA,0.65,NA,NA,NA,NA,NA,16,3.8,300,NA,1797.79220613579,NA,55,17.8994949366117,369.65463530487,NA,2,1,2.56066017177982,45.2015331370399,2,14.2101551083915,2,NA,NA,10,0.4,0.2,NA,NA,1.01,NA,0.01,NA,NA,NA,NA,NA,0.1,0.66,6
"PER005","PER005","South America","Andes Central","Peru","Arequipa","Alca","Alca-3","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-15.12,-72.69,"","","","","Obsidian","""Alca-1 obsidian was heavily used in the Department of Cuzco, and is seldom found outside of it. Its location is still unknown but assumed to be in the Southern Highlands, and it was (probably) used during the Preceramic (Asaro and Burger 1997).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Robert J. Speakman, and Richard L. Burger. Sources of Archaeological Obsidian in Peru: Description and Geochemistry. American Chemical Society Symposium Series: Chapter 28, (2007) 522-552. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,33100,NA,32850,NA,1269,561.5,7953,NA,54,11,126,257,15,150.5,9,NA,NA,1018,36.2,69.2,NA,NA,2,NA,0.68,NA,NA,NA,NA,NA,13.5,2.76,200,NA,1579.59415460184,NA,94,20.2677669529664,185.089357775095,NA,5.74264068711928,1,1.95710678118655,51.5477272147525,3,13.2175144212722,2,NA,NA,3,0.1,0.1,NA,NA,0.24,NA,0.01,NA,NA,NA,NA,NA,0.1,0.6,6
"PER013","PER013","South America","Andes Central","Peru","Puno","Macusani","Macusani-A","5.5","",5.5,"","Active","Convergent","Continental","Active Continental Margin",-13.995,-70.283,"","","","","Obsidian","""Macusani obsidian varies from 'translucent-green, opaque milky-green, translucent pale yellow, or opaque red-brown spots irregularly dispersed in a translucent-green matrix.' Milky-green samples contain many irregular shaped fluid inclusions.While the bulk of this obsidian formed around 5.5 mya in a volcanic event that formed the Macusani Basin, there are a few deposits that formed later in time. Macusani 1 occurs in larger clast sizes than Macuani 2, and comes from deposits near Chilcuno Chico and Caluyo Mayo (Craig et al 2009).""","","""Literature suggests alternate names for this source include: Macusani 1, Paucartambo glass (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Craig, Nathan, Robert J. Speakman, Rachel S. Popelka-Filcoff, Mark Aldenderfer, Luis Flores Blanco, Margaret Brown Vega, Michael D. Glascock, and Charles Stanish. Macusani Obsidian from Southern Peru: A Characterization of its Elemental Composition with a Demonstration of its Ancient Use. Journal of Archaeological Science 37 (2010) 569-576. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,473,4349,NA,NA,NA,1177,5,NA,8,37,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,56,97,NA,NA,NA,22,1,NA,2,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"PER014","PER014","South America","Andes Central","Peru","Puno","Macusani","Macusani-B","5.5","",5.5,"","Active","Convergent","Continental","Active Continental Margin",-14.637,-69.352,"","","","","Obsidian","""Macusani obsidian varies from 'translucent-green, opaque milky-green, translucent pale yellow, or opaque red-brown spots irregularly dispersed in a translucent-green matrix.' Milky-green samples contain many irregular shaped fluid inclusions.While the bulk of this obsidian formed around 5.5 mya in a volcanic event that formed the Macusani Basin, there are a few deposits that formed later in time. Macusani 2 occurs in smaller clast sizes than Macusani 1, and comes from deposits near Chapi (Craig et al 2009).""","","""Literature suggests alternate names for this source include: Macusani 2, Paucartambo glass (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Craig, Nathan, Robert J. Speakman, Rachel S. Popelka-Filcoff, Mark Aldenderfer, Luis Flores Blanco, Margaret Brown Vega, Michael D. Glascock, and Charles Stanish. Macusani Obsidian from Southern Peru: A Characterization of its Elemental Composition with a Demonstration of its Ancient Use. Journal of Archaeological Science 37 (2010) 569-576. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,614,3282,NA,NA,NA,1357,8,NA,6,34,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,59,68,NA,NA,NA,26,1,NA,3,3,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,6
"PER027","PER027","South America","Andes Central","Peru","Ayacucho","Wimpilla","Wimpilla A","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-15.003,-73.405,"LOCATION IS UNKNOWN AND APPROXIMATED","","","","Obsidian","","""The use of this obsidian is rare in archaeological contexts (Asaro and Burger 1977).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Burger, Richard L. and Frank Asaro. Trace Element Analysis of Obsidian Artifacts from the Andes: New Perspectives on Pre-Hispanic Economic Interaction in Peru and Bolivia. Archaeological Research Facility, UC Berkeley, 1977. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,311,5700,NA,NA,NA,81,NA,NA,NA,NA,0.52,2.51,1194,24.5,NA,NA,NA,7.68,5.88,0.547,5.67,NA,4.07,0.8,NA,7.66,3.08,NA,NA,NA,0.03,NA,6,200,NA,NA,NA,4,NA,NA,NA,NA,0.08,0.13,28,0.8,NA,NA,NA,0.11,0.02,0.01,0.06,NA,0.08,0.01,NA,0.07,0.04,1
"PER028","PER028","South America","Andes Central","Peru","Ayacucho","Wimpilla","Wimpilla B","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-15.003,-73.405,"LOCATION IS UNKNOWN AND APPROXIMATED","","","","Obsidian","","""The use of this obsidian is rare in archaeological contexts (Asaro and Burger 1977).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Burger, Richard L. and Frank Asaro. Trace Element Analysis of Obsidian Artifacts from the Andes: New Perspectives on Pre-Hispanic Economic Interaction in Peru and Bolivia. Archaeological Research Facility, UC Berkeley, 1977. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,412,6900,NA,NA,NA,241,NA,NA,NA,NA,0.06,6.32,574,47.1,NA,NA,NA,2.36,3.44,0.528,1.74,NA,4.68,1.48,NA,35.08,8.33,NA,NA,NA,0.02,NA,8,200,NA,NA,NA,5,NA,NA,NA,NA,0.04,0.16,19,0.9,NA,NA,NA,0.08,0.01,0.009,0.03,NA,0.08,0.01,NA,0.22,0.06,1
"MEX064","MEX064","North America","Trans-Mexican Volcanic Belt","Mexico","Michoacán","Cerro Varal","Cerro Varal-2","","",NA,"","Active","Convergent","Continental","Active Continental Margin",19.862,-101.768,"","Michoacán-Guanajuato Volcanic Field","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UWA008","UWA008","North America","","USA","Washington","Copper Mountain","Copper Ridge C","","",NA,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","Garibaldi Volcanic Belt or Cascade Arc","Low","Obsidian","""Nearly all Washington obsidian is thought to be low quality, and largely unused for tool manufacture' (Gallagher 2016).""","",""" Literature suggests alternate names for this source include: Copper Ridge #3 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gallagher, Anna. The Binderbost Site: Exploring Migration and Trade on the Social Landscape of the Pacific Northwest. University of Pittsburgh 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR005","UOR005","North America","Great Basin","USA","Oregon","Beatys Butte","Beatys Butte A","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",42.394,-119.324,"","","High Lava Plains","High","Obsidian","""Dense concentrations of surface nodules covering several square kilometers are found on the lower northern,
eastern, and western slopes of Beatys Butte and are common in the lacustrine deposits of Pluvial Lake Catlow
to the north and east of the butte. Obsidian from this source was widely used in the Steens Mountain area and
the southeastern portion of the state and has been identified as far north as the Malheur National Forest and as
far west as the southern Oregon coast' Skinner and Thatcher 2003).""","","""Literature suggests alternate names for this source include: Beaty's Butte, Beatty's Butte (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"MEX033","MEX033","North America","Trans-Mexican Volcanic Belt","Mexico","Hidalgo","Sierra de Pachuca","Sierra de Pachuca-1","","14.5-5",9.75,"","Active","Convergent","Continental","Active Continental Margin",20.143,-98.751,"LOCATION ONLY","","Eastern TMVB","High","Obsidian","""Pachuca obsidian is transparent green with a green-gold tint. The glass is of fine quality for tool making and contains very few inclusions (Doering 2002).""","""Pachuca was one of the earliest sources exploited in Central Mexico, with blades associated with mammoth kill sites in the Late Pleistocene (Doering 2002).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ferrari, Luca, Teresa Orozco-Esquivel, Vlad Manea, Marina Manea. The Dynamic History of the Trans-Mexican Volcanic Belt and the Mexico Subduction Zone. Tectonophysics 522-523 (2012) 122-149. ; Doering, Travis F. Obsidian Artifacts from San Andres, La Venta, Tabasco, Mexico. The Florida State University, 2002.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN016","JPN016","Eurasia","Japan","Japan","Hokkaido","Ikutahara","Ikutahara Group General","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.689,143.556,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ECU003","ECU003","South America","Andes North","Ecuador","Pichincha","Callejones","Callejones-1","0.22-0.01","",0.115,"","","","Continental","Active Continental Margin",-0.223,-78.46,"","Sierra de Guamani","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Knight, Charles L. F., Andrea M. Cuellar, Michael D. Glascock, Minard L. Hall, and Patricia A. Mothes. Obsidian Source Characterization in the Cordillera Real and Eastern Piedmont of the North Ecuadorian Andes. Journal of Archaeological Science 38 (2011) 1069-1079.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR077","UOR077","North America","","USA","Oregon","Klamath Marsh","Klamath Marsh 1","","",NA,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR006","UOR006","North America","Great Basin","USA","Oregon","Beatys Butte","Beatys Butte B","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",42.394,-119.324,"","","High Lava Plains","High","Obsidian","""Dense concentrations of surface nodules covering several square kilometers are found on the lower northern,
eastern, and western slopes of Beatys Butte and are common in the lacustrine deposits of Pluvial Lake Catlow
to the north and east of the butte. Obsidian from this source was widely used in the Steens Mountain area and
the southeastern portion of the state and has been identified as far north as the Malheur National Forest and as
far west as the southern Oregon coast' Skinner and Thatcher 2003).""","","""Literature suggests alternate names for this source include: Beaty's Butte, Beatty's Butte (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR058","UOR058","North America","","USA","Oregon","Glass Buttes","Glass Buttes 8","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",43.531,-120.112,"","","High Lava Plains","High","Obsidian","""Nine geochemically distinct sources of obsidian are found in association with the Glass Buttes source complex that is located immediately south of Highway 20 in northeastern Lake County... Secondary deposits of obsidian from this and most other Glass Buttes geochemical source groups occur throughout the basin lying north of the source and in the basin located south of the complex' (Skinner and Thatcher 2003).""","""Although obsidian from all of the identified Glass Buttes sources was primarily used in the immediate region surrounding the source complex, glass from the source area has been identified in archaeological sites to the north in Washington and British Columbia, Canada, and as far west as the Western Cascades of Oregon and the Portland Basin' (Skinner and Thatcher 2003).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ARG056","ARG056","South America","Patagonia","Argentina","Chubut","Telesen","Telesen 2","Mio","",14.25,"Volcanic Field","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",-42.513,-66.964,"","Somuncura Plateau","","","Obsidian","","","","""Stern, Charles R. Obsidian Sources and Distribution in Patagonia, Southernmost South America. Quaternary International xxx (2017) 1-16.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"CHL004","CHL004","South America","Andes South","Chile","Santiago Metropolitan","Laguna del Maule","Laguna del Maule-1 Santiago","","32-10",21,"","","","Continental","Active Continental Margin",-36.044,-70.524,"","","Region of ""Active Margin"" Basins","","Obsidian","""Obsidian from Laguna del Maule comes from the border of Argentina and Chile, as part of the Cordillera Principal Volcanic Complex. Nodules range from 3-5 cm and are heterogenous in composition (Duran et al 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Jordan, Teresa E., W. Matthew Burns, Ricardo Veiga, Francisco Pangaro, Peter Copeland, Shari Kelley, and Constantino Mpodozis. Extension and Basin Formation in the Southern Andes Caused by Increased Convergent Rate: A Mid-Cenozoic Trigger for the Andes. Tectonics 20, 3 (2001) 308-324.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UWA013","UWA013","North America","","USA","Washington","Hosko","Hosko A","","",NA,"","Active","Convergent","Continental","Active Continental Margin",45.952,-120.894,"LOCATION ONLY","","","Low","Obsidian","""Nearly all Washington obsidian is thought to be low quality, and largely unused for tool manufacture' (Gallagher 2016).""","","""Literature suggests alternate names for this source include: Brooks Park, Brooks Memorial State Park (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gallagher, Anna. The Binderbost Site: Exploring Migration and Trade on the Social Landscape of the Pacific Northwest. University of Pittsburgh 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UWA009","UWA009","North America","","USA","Washington","Copper Mountain","Copper Ridge D","","",NA,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","Garibaldi Volcanic Belt or Cascade Arc","Low","Obsidian","""Nearly all Washington obsidian is thought to be low quality, and largely unused for tool manufacture' (Gallagher 2016).""","","""Literature suggests alternate names for this source include: Copper Ridge #4 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gallagher, Anna. The Binderbost Site: Exploring Migration and Trade on the Social Landscape of the Pacific Northwest. University of Pittsburgh 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"RUS002","RUS002","Eurasia","Northeast Asia","Russia","Primorsky Krai","Basaltic Plateau","Basaltic Plateau-1","","",NA,"","Inactive","Convergent","Continental","Active Continental Margin",43.693,132.476,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is the Shoktovo Plateau (Jia et al 2010).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"RUS003","RUS003","Eurasia","Northeast Asia","Russia","Primorsky Krai","Basaltic Plateau","Basaltic Plateau-2","","",NA,"","Inactive","Convergent","Continental","Active Continental Margin",43.693,132.476,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is the Shoktovo Plateau (Jia et al 2010).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"RUS004","RUS004","Eurasia","Northeast Asia","Russia","Primorsky Krai","Basaltic Plateau","Basaltic Plateau-3","","",NA,"","Inactive","Convergent","Continental","Active Continental Margin",43.693,132.476,"","","","","Obsidian","","","""Literature suggests an alternate name for this source is the Shoktovo Plateau (Jia et al 2010).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ARG055","ARG055","South America","Patagonia","Argentina","Chubut","Telesen","Telesen 1","14.6","",14.6,"Volcanic Field","Active","Convergent","Continental","Extensional Zone in Cratonic Continental Interior",-42.513,-66.964,"","Somuncura Plateau","","","Obsidian","","","","""Stern, Charles R. Obsidian Sources and Distribution in Patagonia, Southernmost South America. Quaternary International xxx (2017) 1-16.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UCA057","UCA057","North America","","USA","California","Saline Range","Saline Range Variety 3","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","Miocene Volcanism Arc Axes","","Obsidian","""The Saline Range is composed of a volcanic tableland, separating the Saline Valley from Eureka Valley in California. The obsidian nodules found here are eroded out from rhyolitic flows and tuffs, mixing into alluvial deposits and transported as far away as 20 km. Primary outcrops for Saline Ranges 1, 2, and 3 can often be found in close proximity to each other on the east side of the ridge. Obsidian sources here exhibit a high degree of translucency with a gold-brown cast, occasionally containing tight, parallel black banding. Saline Ranges 2 and 3 often feature unpatterned and blotchy clouded areas (Giambastiani 2004).""","","""Literature suggests alternate names for this source include: Dry Mountain, Saline Range (Variety 3), Saline Valley, Saline Valley 3 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"TNZ001","TNZ001","Africa","African Rift","Tanzania","Kilimanjaro","Mt. Kilimanjaro","Mt. Kilimanjaro #1","","2.6-0",1.3,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",NA,NA,"","Kilimanjaro","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ETH010","ETH010","Africa","African Rift","Ethiopia","Ethiopia","Axum","Axum A","","",NA,"","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",NA,NA,"","","Main Ethiopia RIft","","Obsidian","","","""Literature suggests alternate names for this source include: Askum A, AxuM A (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ETH011","ETH011","Africa","African Rift","Ethiopia","Ethiopia","Axum","Axum D","","",NA,"","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",NA,NA,"","","Main Ethiopia RIft","","Obsidian","","","""Literature suggests alternate names for this source include: Askum D, AxuM D (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ECU004","ECU004","South America","Andes North","Ecuador","Pichincha","Callejones","Callejones-2","0.22-0.01","",0.115,"","","","Continental","Active Continental Margin",-0.223,-78.46,"","Sierra de Guamani","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Knight, Charles L. F., Andrea M. Cuellar, Michael D. Glascock, Minard L. Hall, and Patricia A. Mothes. Obsidian Source Characterization in the Cordillera Real and Eastern Piedmont of the North Ecuadorian Andes. Journal of Archaeological Science 38 (2011) 1069-1079.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR067","UOR067","North America","","USA","Oregon","Horse Mountain","Horse Mountain Variety 2","","12-2",7,"","Hotspot","Intraplate","Continental","Extensional Zone in Cratonic Continental Interior",NA,NA,"","","High Lava Plains","","Obsidian","","","""Literature suggests alternate names for this source include: Horse Mountain B (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Egger, Anne E. and Elizabeth L. Miller. Evolution of the Northwestern Margin of the Basin and Range: The Geology and Extensional History of the Warner Range and Environs, Northeastern California. Geosphere 7, 3 (2011) 756-773.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ARM019","ARM019","Eurasia","Persian Belt","Armenia","Syunik","Satanakar","Satanakar Group General","","23-2.6",12.8,"","Inactive","Convergent","Continental","Active Continental Margin",39.803,45.784,"","Syunik","","","Obsidian","","","""Literature suggests alternate names for this source include: Metz Satanakar (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR100","UOR100","North America","","USA","Oregon","Quartz Mountain","Quartz Mountain A","","2.6",2.6,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","High","Obsidian","","","""Literature suggests alternate names for this source include: Dry Butte, Rogers Butte (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ;""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR101","UOR101","North America","","USA","Oregon","Quartz Mountain","Quartz Mountain B","","2.6",2.6,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","High","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN113","JPN113","Eurasia","Japan","Japan","Nagano","Wadatouge","Wadatouge Group General","","",NA,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"PER024","PER024","South America","Andes Central","Peru","Ayacucho","Wimpilla","Wimpilla Group General","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",-15.003,-73.405,"LOCATION IS UNKNOWN AND APPROXIMATED","","","","Obsidian","","""The use of this obsidian is rare in archaeological contexts (Asaro and Burger 1977).""","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Baker, M. C. W., and P. W. Francis. Upper Cenozoic Volcanism in the Central Andes - Ages and Volumes. Earth and Planetary Science Letters 41 (1978) 175-187.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"KEN028","KEN028","Africa","African Rift","Kenya","Kenya","Mount Kenya","Mount Kenya Group General","","",NA,"","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",-0.116,37.294,"","Mount Kenya","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Ebinger, C. J. and N. H. Sleep. Cenozoic Magmatism Throughout East Africa Resulting from the Impact of a Single Plume. Nature 395 (1998) 788-791.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UCA011","UCA011","North America","Great Basin","USA","California","Casa Diablo","Casa Diablo Lookout Mountain subsource","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.581,-118.547,"","","Miocene Volcanism Arc Axes","Medium","Obsidian","""Casa Diablo is one of the largest sources of obsidian in the southwest, and is located in the Long Valley Caldera, California. There are between 16-26 subsources found over 65 square km, all of varying sizes and color. Obsidian here is primarily in the form of cobbles and boulders, reaching as large as one meter in length. Textures of Casa Diablo are glassy, but may exhibit fine-grained surfaces with occasional phenocryst inclusions (Giambastiani 2004).""","""There are four major outcrops used historically: Lookout Mountain, Dry Creek Canyon, Sawmill Ridge, and Obsidian Hill (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Casa Diablo, Lookout Mountain (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Rick, Torben C., Craig E. Skinner, Jon M. Erlandson, and René L. Vellanoweth. Obsidian Source Characterization and Human Exchange Systems on California's Channel Islands. Pacific Coast Archaeological Society Quarterly 37, 3 (2001) 27-44. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UCA013","UCA013","North America","Great Basin","USA","California","Casa Diablo","Casa Diablo Sawmill Ridge subsource","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.581,-118.547,"","","Miocene Volcanism Arc Axes","Medium","Obsidian","""Casa Diablo is one of the largest sources of obsidian in the southwest, and is located in the Long Valley Caldera, California. There are between 16-26 subsources found over 65 square km, all of varying sizes and color. Obsidian here is primarily in the form of cobbles and boulders, reaching as large as one meter in length. Textures of Casa Diablo are glassy, but may exhibit fine-grained surfaces with occasional phenocryst inclusions (Giambastiani 2004).""","""There are four major outcrops used historically: Lookout Mountain, Dry Creek Canyon, Sawmill Ridge, and Obsidian Hill (Giambastiani 2004).""","""Literature suggests alternate names for this source include: Casa Diablo, Sawmill Ridge (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Moore, Joe. Great Basin Tool-Stone Sources. Nevada Department of Transportation (2009) 24-42. ; Rick, Torben C., Craig E. Skinner, Jon M. Erlandson, and René L. Vellanoweth. Obsidian Source Characterization and Human Exchange Systems on California's Channel Islands. Pacific Coast Archaeological Society Quarterly 37, 3 (2001) 27-44. ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UCA062","UCA062","North America","Cascadia","USA","California","Paradise Ridge","Paradise Ridge Group General","","42-0",21,"","Active","Convergent","Continental","Active Continental Margin",36.766,-121.637,"","","Cascade Arc","","Obsidian","","","""Literature suggests alternate names for this source include: Paradise Ridge 1-2, Tuscan (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Madsen, J. K., D. J. Thorkelson, R. M. Friedman, and D. D. Marshall. Cenozoic to Recent Plate Configurations in the Pacific Basin: Ridge Subduction and Slab Window Magmatism in Western North America. Geosphere 2, 1 (2006) 11-34.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN009","JPN009","Eurasia","Japan","Japan","Kanagawa","Hakone","Hakone Group General","","2.6",2.6,"","Active","Convergent","Continental","Mature Island Arc",35.245,139.079,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN012","JPN012","Eurasia","Japan","Japan","Oita","Himeshima","Himeshima Group General","","2.6",2.6,"","Active","Convergent","Continental","Mature Island Arc",33.73,131.671,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ECU006","ECU006","South America","Andes North","Ecuador","Napo","Consanga","Cosanga-A","0.54-0.0006","",0.2703,"","","","Continental","Active Continental Margin",-1.052,-77.825,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Pumayacu, Río Consanga (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ARG004","ARG004","South America","Andes Central","Argentina","Jujuy","Caldera Vilama","Caldera Vilama-2","","",NA,"","Active","Convergent","Continental","Active Continental Margin",-22.5533,-66.687,"LOCATION ONLY","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UOR078","UOR078","North America","","USA","Oregon","Klamath Marsh","Klamath Marsh 2","","",NA,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UNV034","UNV034","North America","Great Basin","USA","Nevada","Meadow Valley Mountains Vitrophyre","Meadow Valley Mountains Vitrophyre Group","","10-5.3",7.65,"Pyroclastic Volcanogenic Basin","Active","Convergent","Continental","Active Continental Margin",37.101,-114.66,"","","Miocene Volcanism Arc Axes","","Obsidian","""Meadow Valley Mountain obsidian is a uniform opaque black that may contain phenocrysts, and is composed of four subsources (Haarklau et al 2005).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Haarklau, Lynn, Lynn Johnson, and David L. Wagner. Fingerprints in The Great Basin: The Nellis Air Force Base Regional Sourcing Study. US Army Corps of Engineers, Fort Worth District (2005). ; Noble, Donald C. Some Observations on the Cenozoic Volcano-Tectonic Evolution of the Great Basin, Western United States. Earth and Planetary Science Letters 17 (1972) 142-150. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"MEX083","MEX083","North America","Trans-Mexican Volcanic Belt","Mexico","Zacatecas","Huitzila","Huitzila-1","","10",10,"","Active","Convergent","Continental","Active Continental Margin",21.211,-103.611,"","","Western TMVB","High","Obsidian","""Huitzila is high quality obsidian and is found in many colors - including 'rainbow' varieties. The source was heavily exploited during pre-Hispanic times (Glascock et al 2010).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Phil C. Weigand, Rodrigo Esparza López, Michael A. Ohnersorgen, Mauricio Garduño, Joseph B. Mountjoy, and J. Andrew Darling. Geochemical Characterisation of Obsidian in Western Mexico: the Sources in Jalisco, Nayarit, and Zacatecas. Crossing the Straits: Prehistoric Obsidian Source Exploitation in the North Pacific Rim, edited by Yaroslav V. Kuzmin and Michael D. Glascock. (2010) 201-208.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"MEX084","MEX084","North America","Trans-Mexican Volcanic Belt","Mexico","Zacatecas","Huitzila","Huitzila-2","","10",10,"","Active","Convergent","Continental","Active Continental Margin",21.211,-103.611,"","","Western TMVB","High","Obsidian","""Huitzila is high quality obsidian and is found in many colors - including 'rainbow' varieties. The source was heavily exploited during pre-Hispanic times (Glascock et al 2010).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Glascock, Michael D., Phil C. Weigand, Rodrigo Esparza López, Michael A. Ohnersorgen, Mauricio Garduño, Joseph B. Mountjoy, and J. Andrew Darling. Geochemical Characterisation of Obsidian in Western Mexico: the Sources in Jalisco, Nayarit, and Zacatecas. Crossing the Straits: Prehistoric Obsidian Source Exploitation in the North Pacific Rim, edited by Yaroslav V. Kuzmin and Michael D. Glascock. (2010) 201-208.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UWA001","UWA001","North America","Cascadia","USA","Washington","Agnes Creek","Agnes Creek A","","",NA,"","Active","Convergent","Continental","Active Continental Margin",48.188,-120.961,"LOCATION ONLY","","","Low","Obsidian","""Nearly all Washington obsidian is thought to be low quality, and largely unused for tool manufacture' (Gallagher 2016).""","","""Literature suggests alternate names for this source include: Agnes Creek (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gallagher, Anna. The Binderbost Site: Exploring Migration and Trade on the Social Landscape of the Pacific Northwest. University of Pittsburgh 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UWA002","UWA002","North America","Cascadia","USA","Washington","Agnes Creek","Agnes Creek B","","",NA,"","Active","Convergent","Continental","Active Continental Margin",48.188,-120.961,"LOCATION ONLY","","","Low","Obsidian","""Nearly all Washington obsidian is thought to be low quality, and largely unused for tool manufacture' (Gallagher 2016).""","","""Literature suggests alternate names for this source include: Agnes Creek (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gallagher, Anna. The Binderbost Site: Exploring Migration and Trade on the Social Landscape of the Pacific Northwest. University of Pittsburgh 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"CHL005","CHL005","South America","Andes South","Chile","Santiago Metropolitan","Laguna del Maule","Laguna del Maule-2 Santiago","","32-10",21,"","","","Continental","Active Continental Margin",-36.044,-70.524,"","","Region of ""Active Margin"" Basins","","Obsidian","""Obsidian from Laguna del Maule comes from the border of Argentina and Chile, as part of the Cordillera Principal Volcanic Complex. Nodules range from 3-5 cm and are heterogenous in composition (Duran et al 2011).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Jordan, Teresa E., W. Matthew Burns, Ricardo Veiga, Francisco Pangaro, Peter Copeland, Shari Kelley, and Constantino Mpodozis. Extension and Basin Formation in the Southern Andes Caused by Increased Convergent Rate: A Mid-Cenozoic Trigger for the Andes. Tectonics 20, 3 (2001) 308-324.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ICE008","ICE008","Eurasia","Atlantic","Iceland","Iceland","Kviarjokull","Kviarjokull A","","",NA,"","Active","Divergent","Oceanic","Extensional Zone in Oceanic Basin",NA,NA,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"TNZ002","TNZ002","Africa","African Rift","Tanzania","Kilimanjaro","Mt. Kilimanjaro","Mt. Kilimanjaro #2","","2.6-0",1.3,"Stratovolcano","Active","Divergent","Continental","Extensional Zone in Cratonic Continental Interior",NA,NA,"","Kilimanjaro","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Global Volcanism Program, 2013. Volcanoes of the World, v. 4.6.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 4 Oct 2017. http://dx.doi.org/10.5479/si.GVP.VOTW4-2013.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UNV013","UNV013","North America","","USA","Nevada","Cloverdale Canyon","Cloverdale Canyon A","","",NA,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Group 1 (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UNV014","UNV014","North America","","USA","Nevada","Cloverdale Canyon","Cloverdale Canyon B","","",NA,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"UWA014","UWA014","North America","","USA","Washington","Hosko","Hosko B","","",NA,"","Active","Convergent","Continental","Active Continental Margin",45.952,-120.894,"LOCATION ONLY","","","Low","Obsidian","""Nearly all Washington obsidian is thought to be low quality, and largely unused for tool manufacture' (Gallagher 2016).""","","""Literature suggests alternate names for this source include: Brooks Park, Brooks Memorial State Park (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Gallagher, Anna. The Binderbost Site: Exploring Migration and Trade on the Social Landscape of the Pacific Northwest. University of Pittsburgh 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ECU007","ECU007","South America","Andes North","Ecuador","Napo","Consanga","Cosanga-B","0.54-0.0006","",0.2703,"","","","Continental","Active Continental Margin",-1.052,-77.825,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Pumayacu, Río Consanga (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"MEX063","MEX063","North America","Trans-Mexican Volcanic Belt","Mexico","Michoacán","Cerro Varal","Cerro Varal-1","","",NA,"","Active","Convergent","Continental","Active Continental Margin",19.862,-101.768,"","Michoacán-Guanajuato Volcanic Field","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN038","JPN038","Eurasia","Japan","Japan","Nagano","Omegura","Omegura Group General","","23",23,"","Active","Convergent","Continental","Mature Island Arc",36.0313,138.365,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Wada I and II (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"TKY012","TKY012","Eurasia","Persian Belt","Turkey","Nevsehir","Hotamis Dag","Hotamis Dag Group General","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",38.537,34.626,"","","","","Obsidian","""There are five subsources in the Hotamis Dag group: Acigöl (wall of the maar), Acigöl-Bogazköy (the wall of the caldera), Acigöl-Güney Dagi, Acigöl-Kocadag, and Acigöl-Taskesiktepe (Oddone et al 1997).""","","""Literature suggests alternate names for this source include: Acigöl (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"TKY016","TKY016","Eurasia","Persian Belt","Turkey","Turkey","Kars Arpacay","Kars Arpacay A","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"TKY017","TKY017","Eurasia","Persian Belt","Turkey","Turkey","Kars Arpacay","Kars Arpacay B","","23-2.6",12.8,"","Active","Convergent","Continental","Active Continental Margin",NA,NA,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Dilek, Yildirium, NazimImamcerdiyev, and Safak Altunkaynak. Geochemistry and Tectonics of Cenozoic Volcanism in the Lesser Caucasus (Azerbaijan) and the Peri-Arabian Region: Collision-Induced Mantle Dynamics and its Magmatic Fingerprint. International Geology Review 52, 4-6 (2010) 536-578.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ARM016","ARM016","Eurasia","Persian Belt","Armenia","Kotayk","Hatis","Hatis Group General","","23",23,"","Inactive","Convergent","Continental","Active Continental Margin",40.495,44.68,"","Gegham","","","Obsidian","","","""Literature suggests alternate names for this source include: Atis, Akunk deposit (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Sosson, M., Y. Rolland, C. Muller, T. Danelian, R. Melkonyan, S. Kekelia, S. Adamia, V. Babazadeh, T. Kangarli, A. Avagyan, G. Galoyan, and J. Mosar. Subductions, Obductions, and Collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), New Insights. Geological Society, London, Special Publications 340 (2010) 329-352.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"TKY034","TKY034","Eurasia","Persian Belt","Turkey","Bitlis","Süphaun Dag","Süphaun Dag I","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",38.931,42.829,"","Lake Van Volcanic Area","","","Obsidian","","","""Literature suggests alternate names for this source include: Mount Süphan (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Innocenti, F., R. Mazzuoli, G. Pasquare, F. Radicati di Brozolo, and L. Villari. Evolution of the Volcanism in the Area of Interaction Between the Arabian, Anatolian, and Iranian Plates (Lake Van, Eastern Turkey). Journal of Volcanology and Geothermal Research 1 (1976) 103-112. ; Carter, Tristan, Sarah Grant, Metin Kartal, Aytaç Coşkun, and Vecihi Özkaya. Networks and Neolithisation: Sourcing from Kortik Tepe (SE Anatolia). Journal of Archaeological Science 40 (2013) 556-569.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"TKY035","TKY035","Eurasia","Persian Belt","Turkey","Bitlis","Süphaun Dag","Süphaun Dag II","","23-0",11.5,"","Active","Convergent","Continental","Active Continental Margin",38.931,42.829,"","Lake Van Volcanic Area","","","Obsidian","","","""Literature suggests alternate names for this source include: Mount Süphan (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Innocenti, F., R. Mazzuoli, G. Pasquare, F. Radicati di Brozolo, and L. Villari. Evolution of the Volcanism in the Area of Interaction Between the Arabian, Anatolian, and Iranian Plates (Lake Van, Eastern Turkey). Journal of Volcanology and Geothermal Research 1 (1976) 103-112.""",1,1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN025","JPN025","Eurasia","Japan","Japan","Tokyo","Kouzushima","Kouzushima Group General","","23-2.6",12.8,"","Active","Convergent","Continental","Mature Island Arc",34.425,139.285,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"RPN003","RPN003","Pacific","Pacific","Chile","Easter Island","Rano Kau","Rano Kau I","","0.3-0",0.15,"Shield","Active","Divergent","Oceanic","Extensional Zone in Oceanic Basin",-27.178,-109.439,"","","","","Obsidian","","","""Literature suggests alternate names for this source include: Rano Kau NW (IAOS World Source Catalog).""","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Bonatti, E., C. G. A. Harrison, D. E. Fisher, J. Honnorez, J.-G. Schilling, J. J. Stipp, and M. Zentilli. Easter Volcanic Chain (Southeast Pacific): A Mantle Hot Line. Journal of Geophysical Research 82, 17 (1977) 2457-2478.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN036","JPN036","Eurasia","Japan","Japan","Shimane","Oki","Oki Group General","","2.6",2.6,"","Active","Convergent","Continental","Mature Island Arc",36.296,133.244,"","","","","Obsidian","""There are six geochemically unique subsources in the Oki group (Watanabe and Suzuki 2009).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Watambe, K and M. Suzuki. Analytical Data of Geologic Obsidians from Japan by INAA Using Middle- and Long-lived Nuclides. Journal of Analytical and Nuclear Chemistry 279, 2 (2009) 459-473 ; Matsuda, T., K, Nakamura, and A. Sugimura. Late Cenozoic Orogeny in Japan. Technophysics 4, 4-6 (1967) 349-366.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"JPN002","JPN002","Eurasia","Japan","Japan","Hokkaido","Asahikawa","Asahikawa Group General","","",NA,"","Active","Convergent","Continental","Mature Island Arc",43.778,142.269,"","","","","Obsidian","""There are two subsources for this glass - Asahikawa-Higashitakasu and Asahikawa-Syunkodai (Lynch et al 2016).""","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html. ; Lynch, Sean C., Hirofumi Kato, and Andrzej W. Weber. Obsidian Resource Use From Jomon to Oshotsk Period on Rebun Island: An Analysis of Archaeological Obsidian. Journal of Archaeological Science 2016.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ICE009","ICE009","Eurasia","Atlantic","Iceland","Iceland","Kviarjokull","Kviarjokull B","","",NA,"","Active","Divergent","Oceanic","Extensional Zone in Oceanic Basin",NA,NA,"","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA
"ARG003","ARG003","South America","Andes Central","Argentina","Jujuy","Caldera Vilama","Caldera Vilama-1","","",NA,"","Active","Convergent","Continental","Active Continental Margin",-22.5533,-66.687,"LOCATION ONLY","","","","Obsidian","","","","""International Association for Obsidian Studies: World Obsidian Source Catalog. IAOS World Obsidian Source Catalog, Northwest Research and the Archaeometry Laboratory at MURR, www.sourcecatalog.com/sourcecatalog/s_home.html.""",1,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA