This was one of a series of requests to image a group of cones with summit depressions along the north wall of Coprates Chasma. There are also “breached” cones and cones with flows, which we can all compare. Can they inferred to be volcanic, or perhaps an erosion or inversion of topography?
ID:
ESP_036109_1675date: 10 April 2014
altitude: 266 km
https://uahirise.org/hipod/ESP_036109_1675
NASA/JPL-Caltech/University of Arizona
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