Coprates Catena is a chain of collapsed structures, which run parallel to the main valley Coprates Chasma.
These collapsed structures vary between 2500 and 3000 metres deep, which is far less than the depth of the main valley at 8000 metres. A few landslides can be seen on the valley walls.
The valley chains have no connection to the lowland plains as compared to the main valleys. This indicates that their origin is solely due to the expansion of the surface, or collapse, with removal of underlying material (possibly water or ice).
On the valley floor, brighter layers are exposed, which could be material of the same composition as seen in other parts of Valles Marineris, where sulphates have been measured by the OMEGA spectrometer instrument on board Mars Express.
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| | Crater Hale in Argyre basin (http://www.esa.int/SPECIALS/Mars_Express/SEM8AVWJD1E_0.html) |
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| | Olympus Mons caldera in perspective (http://www.esa.int/SPECIALS/Mars_Express/SEMKC2W4QWD_0.html) |
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| | View of deposits in Melas Chasma on Mars (http://www.esa.int/SPECIALS/Mars_Express/SEMFKTV4QWD_0.html) |
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