Sisyphi Montes and Southwest Hellas Paterae: Possible Impact, Cryotectonic, Volcanic, and Mantle Tectonic Processes and Hellas Basin Rings

Details Sisyphi Montes and Southwest Hellas Paterae: Possible Impact, Cryotectonic, Volcanic, and Mantle Tectonic Processes and Hellas Basin Rings Sisyphi Montes and Southwest Hellas Paterae: Possible Impact, Cryotectonic, Volcanic, and Mantle Tectonic Processes and Hellas Basin Rings

Oct 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpico1323.8066r&link_type=abstract

Fourth International Conference on Mars Polar Science and Exploration, October 2-6, 2006, Davos, Switzerland. LPI Contribution

Physics

Scientific paper

Sisyphi Montes appear to be volcanoes that emerged from the central
zones of impact craters distributed along Hellas structural rings.
Subsequent, volatile-driven resurfacing along the impact structures may
explain the formation of peripheral moats.

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