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[edit] Summary
NASA
http://www.nasa.gov/mission_pages/MRO/multimedia/pia09189.html
Ridges as Evidence of Fluid Alteration
Tectonic fractures within the Candor Chasma region of Valles Marineris, Mars, retain ridge-like shapes as the surrounding bedrock erodes away. This points to past episodes of fluid alteration along the fractures and reveals clues into past fluid flow and geochemical conditions below the surface.
[edit] Licensing
This work is in the public domain in the United States because it is a work of the United States Federal Government under the terms of Title 17, Chapter 1, Section 105 of the US Code. See Copyright. Note: This only applies to works of the Federal Government and not to the work of any individual U.S. state, territory, commonwealth, county, municipality, or any other subdivision. |
File history
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Date/Time | Dimensions | User | Comment | |
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current | 01:14, 18 February 2007 | 330×230 (40 KB) | Rickyjames (Talk | contribs) | (NASA http://www.nasa.gov/mission_pages/MRO/multimedia/pia09189.html Ridges as Evidence of Fluid Alteration Tectonic fractures within the Candor Chasma region of Valles Marineris, Mars, retain ridge-like shapes as the surrounding bedrock erodes away. Th) |
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