The deposits on this crater floor are chock full of light-toned deposits, pervasive fracturing and possible dikes. All of this can support the potential for past hydrothermal activity.

ID: PSP_005611_1445
date: 7 October 2007
altitude: 248 km

https://uahirise.org/hipod/PSP_005611_1445
NASA/JPL-Caltech/University of Arizona
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