A portion of the rim of Degas crater is visible towards the top of this image. The hummocky texture of the interior crater wall is due to the slumping and downslope movement of material soon after the crater formed. Date acquired: April 22, 2013Image Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Inst
A portion of the rim of Degas crater is visible towards the top of this image. The hummocky texture of the interior crater wall is due to the slumping and downslope movement of material soon after the crater formed.
Date acquired: April 22, 2013Image Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington