There is a system of curving, inverted features located on the eastern floor of this crater spanning from the north to the south. These 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_064527_1440
date: 2 May 2020
altitude: 247 km

https://uahirise.org/hipod/ESP_064527_1440
NASA/JPL-Caltech/UArizona
#Mars #science #NASA