This mound or mountain may be comprised of a different material than other parts of the Martian surface as it has not eroded as much, and it does not appear to be the result of an impact crater.

ID: ESP_037367_1920
date: 17 July 2014
altitude: 278 km

https://uahirise.org/hipod/ESP_037367_1920
NASA/JPL-Caltech/University of Arizona
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