HiPOD: Friday, 18 October 2019
Channel Possibly Sourced from Impact Crater

Channel Possibly Sourced from Impact Crater

Sourced from an Impact Crater
An impact crater apparently filled and overspilled, creating this impressive channel now populated with sand dunes. But was it seasonal runoff or catastrophic discharge? Note the small, branching channel near the lower left.

ID: ESP_055264_1565
date: 11 May 2018
altitude: 256 km

https://uahirise.org/hipod/ESP_055264_1565
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.