Here on the plains to the west of Juventae Chasma, we see a patch of inverted, or perhaps fluvial, channel forms with superposed or decaying-in-place bedforms that have been acted upon by the wind. This patch is surrounded by a more heavily cratered darker-toned terrain. Is the patch maybe just comprised of sedimentary materials?

ID: ESP_075183_1765
date: 10 August 2022
altitude: 264 km

https://uahirise.org/hipod/ESP_075183_1765
NASA/JPL-Caltech/University of Arizona
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