Origin and evolution of the Valles Marineris region of Mars

The Valles Marineris Region of Mars is located on the eastern flank of the Tharsis bulge which exhibits dramatic landforms that relate in origin to tectonic, volcanic, and geomorphic processes. Tectonic activity due to crustal extension related to the Tharsis-Syria rise (regional doming or lithospheric response to volcanic loading) appears to be the fundamental influence on the canyon formation and evolution. Tectonic activity contributed to deepen the canyon system and competed with erosional and depositional processes that caused canyon to broaden and fill. The primary tectonic processes appear to have been vertical adjustments of crustal blocks under the influence of N-S and E-W extensional stresses. Canyon wall erosional features and landslide morphologies indicate that materials have been transported from the walls to the floor essentially by mass wasting and downfaulting. However, seepage of liquid water or sublimation of ground ice could have contributed to the enlargement of the tributary canyons, thus suggesting that variations in climatic conditions could have accounted for the morphologic evolution of the canyon system.