HiPOD: Saturday, 26 October 2019
Flow in Crater near Reull Vallis

Flow into a Crater near Reull Vallis
It’s a good bet these are indications of glacial flow. Reull Vallis is thought to have formed when running water flowed in the distant past, cutting a steep-sided channel through the Promethei Terra highlands before running on towards the floor of the vast Hellas Basin.

ID: ESP_055276_1385
date: 12 May 2018
altitude: 252 km

https://uahirise.org/hipod/ESP_055276_1385
NASA/JPL-Caltech/UArizona
#Mars #science #NASA

Black & white is less than 5 km across; enhanced color is less than 1 km. For full observation details, visit the ID link.