These formations have been interpreted as mud volcanoes, and a study may help to find out if they bear similarities to other small cones in different regions of Mars, like Ulysses Colles, Hydraotes Colles and on the bottom of Coprates Chasma. Could they have all formed by same processes or not?
ID:
ESP_076593_1990date: 28 November 2022
altitude: 284 km
https://uahirise.org/hipod/ESP_076593_1990
NASA/JPL-Caltech/University of Arizona
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