Also available in Context Camera image data, the objective of this observation is to examine layers at the base of mounds The extensive network of ridges in the Aeolis region is interpreted as having formed by topographic inversion of fluvial and alluvial deposits.
ID:
ESP_076217_1785date: 30 October 2022
altitude: 269 km
https://uahirise.org/hipod/ESP_076217_1785
NASA/JPL-Caltech/University of Arizona
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