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Interpreting Crater Shadows

fermigas edited this page Oct 13, 2018 · 4 revisions

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Description

The average shape of fresh craters on the Moon is thought to change systematically with diameter in a manner summarized in the September 23, 2004 LPOD. Craters with diameters less than about 10 km are said to be predominantly "simple" craters with bowl-like shapes; where "bowl" can evidently mean having either straight (conical) or curved (spherical or parabolic) walls, and with or without a flat portion of floor in the center. This page shows how Albategnius C appears when illuminated at a various sun angles, and compares the images to what would be expected with those lighting conditions for a pair of simple shapes generated with the Crater Shadows Simulator utility program.

Albategnius C

This a Albategnius C as it appears in a low resolution scan of Apollo Panoramic image AS16-P-4640 :
Albategnius_C_AS16-P-4640.jpg
It appears there may be a small flat section to the floor, but the resolution of the scan is not adequate to be sure.

Here are its contours as interpreted on LTO map 77-C1 :
Albategnius_C_LTO77C1.jpg
The contours within the crater bowl seem to have been drawn with a constant spacing indicating a constant slope, although this may be reading more into the chart than was originally intended.

And here is a comparison of the observed shadow patterns at various sun angles and the patterns that would be expected for a spherical versus a conical shape. The images are mostly moderate resolution scans from the LPI (such as Apollo AS16-M-0708, plus the center image from Lunar Orbiter IV (frame 101H) :
Albategnius_C_shadow_interpretation.JPG
The numbers below the photos are the sun angles. The observed pattern looks much closer to that expected for the conical shape than to that expected for a spherical bowl. The angles available are not adequate to rule out the possibility of a section of flat floor about 1 km in diameter. To reproduce the observed flaring out of the shadow near the top of the rim at high sun angles, the conical shape is not a pure cone, but rather one which has been numerically massaged to give it a bit of extra steepness at the top. LTVT now has the ability to directly record the radial height profile in a crater, so this kind of empirical manipulation of the profile should no longer be necessary.

A Simple Experiment with Shadows - JohnMoore2 JohnMoore2

Bibliography


This page has been edited 4 times. The last modification was made by - JohnMoore2 JohnMoore2 on Jan 18, 2009 4:26 am

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