Colorful Bedrock in the Central Uplift of an Impact Crater – Large impact craters rebound from the initial shock, raising deep bedrock to the surface in the central uplift of the crater. (<a rel="nofollow" class="external text" href="http://www.uahirise.org/ESP_045519_1730">www.uahirise.org/ESP_045519_1730</a>)
<a rel="nofollow" class="external text" href="https://www.flickr.com/people/71688597@N05">UAHiRISE (NASA)</a>
2016-07-13 15:25
<a rel="nofollow" class="external text" href="https://www.flickr.com/photos/uahirise-mars/28049782030/">ESP_045519_1730</a>