This approximately 8 kilometer-diameter impact crater is interesting because of the light-toned band visible in the upper slopes of the inner crater wall.
Because the light-toned materials are confined to a distinct elevation within the crater, it is possible that it represents a well-defined layer exposed in the crater walls.
Written by: L. Crumpler (23 July 2008)
More info and image formats at http://hirise.lpl.arizona.edu/PSP_008792_1410
Image: NASA/JPL/University of Arizona