Title: 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.
Abstract: movement of debris masses and rock-slope material in high-relief terrain, such as scarps and massifs of the dichotomy boundary [e.g., 1-5], impact craters, volcanoes or tectonic grabens as well as scarps in connection with volcanic activity [6] are important estimators for the nearsurface volatile budget and are relevant paleogeomorphic witnesses which help to reconstruct and understand processes involved in the formation of regional landform assemblies. Such deposits can range from deep-seated short-term slumpings to generally slow movement of vo-
Publication Year: 2008
Publication Date: 2008-03-01
Language: en
Type: article
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