This observation shows crater floor material that is differentially eroded, with various units exhibiting divergent geomorphologies throughout the scene. One unit has a lobate form radiating inward from the crater wall: was it once a landslide deposit, now lithified, exhumed, and eroded?

ID: ESP_076165_1585
date: 26 October 2022
altitude: 254 km

https://uahirise.org/hipod/ESP_076165_1585
NASA/JPL-Caltech/University of Arizona
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