This image shows a flow-like feature within Chryse Planitia that is hypothesized to be the result of subsurface sediment mobilization. The flow shows an interesting morphology that might be evidence of the former presence of icy-muddy crust.
ID:
ESP_064868_2005date: 29 May 2020
altitude: 284 km
https://uahirise.org/hipod/ESP_064868_2005
NASA/JPL-Caltech/University of Arizona
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