HiPOD: Sunday, 20 March 2022
Secondary Craters in Bas Relief

Secondary Craters in Bas Relief
This region of Mars has been sprayed with secondary craters from 10-kilometer Zunil Crater to the northwest.

Secondary craters form from rocks ejected at high speed from the primary crater, which then impact the ground at sufficiently high speed to make huge numbers of much smaller craters over a large region. In this scene, however, the secondary crater ejecta has an unusual raised-relief appearance like bas-relief sculpture. How did that happen?

One idea is that the region was covered with a layer of fine-grained materials like dust or pyroclastics about 1 to 2 meters thick when the Zunil impact occurred (about a million years ago), and the ejecta served to harden or otherwise protect the fine-grained layer from later erosion by the wind.

ID: ESP_049076_1845
date: 14 January 2017
altitude: 274 km

https://uahirise.org/hipod/ESP_049076_1845
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.