Carbon dioxide ice has been observed in gullies in this region previously. As time progresses, and the dry ice sublimates away, water ice might be uncovered that can be observed with CRISM instrument. We also want to study any changes in the deposits associated with the gullies. This image is on the southwest outer rim of Asimov Crater.

ID: ESP_065988_1320
date: 24 August 2020
altitude: 252 km

https://uahirise.org/hipod/ESP_065988_1320
NASA/JPL-Caltech/UArizona
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