This locale contains fluvial-like channels in the upland portion which transitions to a broken-up, blocky terrain occupying an amphitheater-shaped valley. This valley is reminiscent of chaos terrain and may indicate collapse due ice table melting. This location may hold clues regarding the relationships between these features and have broader implications for the ice deposit formation throughout the region.
ID:
ESP_072833_2160date: 8 February 2022
altitude: 293 km
https://uahirise.org/hipod/ESP_072833_2160
NASA/JPL-Caltech/University of Arizona
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