This possible volcanic cone with a cratered summit is of interest as an analog to terrestrial cinder cones. Source material for the windblown bedforms around the base are also worth a look. The region appears to be made of many overlapping lava flows, supporting the volcanic origin of this feature.

ID: ESP_063209_1800
date: 20 January 2020
altitude: 262 km

https://uahirise.org/hipod/ESP_063209_1800
NASA/JPL-Caltech/University of Arizona
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