This crater shows an alluvial fan created by a deep valley coming from the west. Thus, a cone-shaped deposit is expected to be in this area. However, there are smaller deposits that run along the northwest wall of the crater. These smaller deposits could be the results of several weak and possibly younger channels.
ID:
ESP_040417_1615date: 11 March 2015
altitude: 256 km
https://uahirise.org/hipod/ESP_040417_1615
NASA/JPL-Caltech/University of Arizona
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