This part of the Ophir Chasma floor is fractured in the north, and in the southern half displays a gentle scarp parallel to the chasm trend, and then a very densely cratered floor zone, possibly related to very old debris aprons. Fracturing and scarp formation may also be related to the formation of the chasm.

ID: ESP_042993_1750
date: 28 September 2015
altitude: 263 km

https://uahirise.org/hipod/ESP_042993_1750
NASA/JPL-Caltech/University of Arizona
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