There are small channels visible in Context Camera data that are of interest at HiRISE resolution. The host crater is (relatively) fresh and thus may be geologically young; the channels incised on both its northern interior rim and floor may be candidates for impact induced hydrothermal activity.

ID: ESP_083444_1440
date: 15 May 2024
altitude: 253 km

https://uahirise.org/hipod/ESP_083444_1440
NASA/JPL-Caltech/University of Arizona
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