The objective of this observation is to examine two flows near the base of a mound near Reull Vallis. There seem to be a number of flows like these in the region. Reull Vallis is believed to have formed when running water flowed in the distant Martian past.

ID: ESP_055065_1405
date: 26 April 2018
altitude: 251 km

https://uahirise.org/hipod/ESP_055065_1405
NASA/JPL-Caltech/University of Arizona
#Mars #science #NASA