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From the lower mapping orbit (50 km) even more details of the landing site are revealed. With the Sun very high in the sky (incidence angle 4°), shadows are minimized and you mostly see variations in albedo (or surface brightness). On the Moon, albedo variations are generally due to either composition (mare vs highlands) or maturity (since fresh, impact-excavated lunar materials tend to have higher albedo, but gradually darken after prolonged exposure to the space environment). Since we're viewing a mare surface far away from highland materials in this image, the albedo variations that you can see are dominantly due to maturity effects. However it is clear from all the LROC landing site images that astronaut activity lowers the albedo, areas of heaviest activity have the lowest albedo, especially around the LM. This effect is most likely due to compaction of a very loose surface powder by simply walking around. The more walking in a given area, the more compaction that takes place, and thus the lower the albedo.
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At the beginning of the first extravehicular activities (EVA) the astronauts learned to walk in 1/6 gravity, unloaded equipment, and setup the camera and flag resulting in a high traffic area that can now be seen from orbit as a low albedo halo surrounding the LM.
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For more information visit http://www.nasa.gov/mission_pages/LRO/multimedia/lroimages/lroc_20091104_apollo12.html
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