At the southern section of the floor of an impact crater is this stunning lobate (tongue-shaped) debris apron with surface banding showing high sinuosity. This is might be the result of glacial or periglacial processes at work in this and possibly other parts of the crater.
ID:
ESP_077210_2140date: 15 January 2023
altitude: 291 km
https://uahirise.org/hipod/ESP_077210_2140
NASA/JPL-Caltech/University of Arizona
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