Complete Makeover

Scaled Image

Image Credit: NASA/JPL/ASU

About this image

The atmosphere of Mars is a dynamic system. Water-ice clouds, fog, and hazes can make imaging the surface from space difficult. Dust storms can grow from local disturbances to global sizes, through which imaging is impossible. Seasonal temperature changes are the usual drivers in cloud and dust storm development and growth. Eons of atmospheric dust storm activity has left its mark on the surface of Mars. Dust carried aloft by the wind has settled out on every available surface; sand dunes have been created and moved by centuries of wind; and the effect of continual sand-blasting has modified many regions of Mars, creating yardangs and other unusual surface forms.
In this image the surface that has been completely modified by the wind. Even the small ridges that remain have been ground down to a cliff-face with a 'tail' of eroded material. The crosshatching shows that the wind regime has remained mainly E/W to ENE/WSW.

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

Context

Image ID: 
V06446025 (View data in Mars Image Explorer)
8.8535
220.974
6446
2003-05-28 22:48
Fri, 2004-07-23
VIS
512 pixels (18 km)
1440 pixels (51 km)
0.035732 km/pixel
0.036189 km/pixel

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