Reconstruction of the Development of Complex Mass-Wasting Landforms at the Western Scarp of Olympus Mons, Mars: Indicators for Talus-derived Landsliding and Post-Emplacement Degradation

Details Reconstruction of the Development of Complex Mass-Wasting Landforms at the Western Scarp of Olympus Mons, Mars: Indicators for Talus-derived Landsliding and Post-Emplacement Degradation Reconstruction of the Development of Complex Mass-Wasting Landforms at the Western Scarp of Olympus Mons, Mars: Indicators for Talus-derived Landsliding and Post-Emplacement Degradation

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.2543v&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Computer Science

Scientific paper

A young complex multi-lobe unit at Olympus Mons has been investigated
indicating a paraglacial origin caused by slope failure and
disintegration of talus deposits.

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