There is a system of curvilinear inverted features located on the eastern floor of this crater spanning from the north to the south. These features might be fluvial in origin. If that is the case, high resolution investigation of these features, including the height at which they stand above the preserved surface around them, will help in determining the hydraulic history of the host crater.

ID: ESP_075619_1445
date: 13 September 2022
altitude: 249 km

https://uahirise.org/hipod/ESP_075619_1445
NASA/JPL-Caltech/University of Arizona
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