High-resolution imaging of this formation will allow detailed analysis of glacial flow and retreat history of this unusually dense moraine assemblage, and how these structures relate to the surface textures of adjacent degraded viscous flow features. Moraines are distinct ridges or mounds of debris that are laid down directly by a glacier or pushed up by it.
ID:
ESP_089855_2215date: 26 September 2025
altitude: 297 km
https://uahirise.org/hipod/ESP_089855_2215
NASA/JPL-Caltech/University of Arizona
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