
Picture taken by the Mars Reconnaissance Orbiter in September 2006.
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.
Recent comments
51 weeks 1 day ago
1 year 10 weeks ago
1 year 21 weeks ago