Cerberus Rupes
About this image
These fractures occur within the volcanic plains south of Elysium Mons. The discontinuation of the fractures - like the one below the main group - indicates that these features are not formed by downdrop of material along faults, but rather formed by the collapse of the ceiling of lava tubes. Small regions of mega-ripples (a dune form) can be seen at the base of the hills at the bottom of the image.
Please see the THEMIS Data Citation Note for details on crediting THEMIS images.
Context
Image ID:
V04326009 (View data in Mars Image Explorer)
10.5918
158.473
4326
2002-12-05 10:34
Thu, 2002-12-19
VIS
1024 pixels (18 km)
3648 pixels (65 km)
0.017955 km/pixel
0.018086 km/pixel