These layers on a canyon wall in Valles Marineris might be either volcanic or sedimentary in origin. This location has been imaged by the Mars Orbiter Camera, and our camera can help to look for boulders and detail structures unresolved by MOC.

ID: ESP_065449_1675
date: 13 July 2020
altitude: 261 km

https://uahirise.org/hipod/ESP_065449_1675
NASA/JPL-Caltech/University of Arizona
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