Hale Crater

Scaled Image

Image Credit: NASA/JPL/ASU

About this image

This VIS image shows part of the floor of Hale Crater. The mountains in the image are part of the elongated central peak of the crater. It is believed that Hale Crater was formed by an oblique impact, which caused its more oval form and central peak elongation.

Please see the THEMIS Data Citation Note for details on crediting THEMIS images. 


Image ID: 
V66105007 (View data in Mars Image Explorer)
2016-11-07 23:04
Fri, 2016-12-16
512 pixels (18 km)
1824 pixels (63 km)
0.034752 km/pixel
0.0352408 km/pixel


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