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  • High-magnitude landslide events on a limestone-scarp in central Germany : morphometric characteristics and climatic controls
  • This paper explores which external climatic variables of difference temporal scales influence the occurrence of high-magnitude landslide events. The investigations were focused on the Wellenkalk-cuesta scarp in the Thuringia Basin. Rainfall
  • Factors controlling mass movement susceptibility on the Wellenkalk-scarp in Hesse and Thuringia
  • of the Wellenkalk and the Röt make the Wellenkalk-scarp one of the most active cuesta slopes in Central Europe with respect to gravitational processes. This study is planned to use the results as a data base for a landslide hazard map of the Thuringia Basin.
  • Talus and pediment flatirons, indicators of climatic change on scarp slopes on the Colorado Plateau, USA