Crater and Channel Infill — There are most likely the remains of glacial processes here. (NASA/JPL/University of Arizona. Acquired: Feb 2017, approximately 254 km above the surface. <a rel="nofollow" class="external text" href="https://www.uahirise.org/ESP_049369_1410">www.uahirise.org/ESP_049369_1410</a>)
<a rel="nofollow" class="external text" href="https://www.flickr.com/people/71688597@N05">UAHiRISE (NASA)</a>
2017-07-04 13:15
<a rel="nofollow" class="external text" href="https://www.flickr.com/photos/uahirise-mars/34897048254/">ESP_049369_1410</a>