Figure 3:


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Temporal sequence of morphodynamic processes and slope stability, phase 1 and 2.
1. The first initial phase is constituted by a completely developed sediment and soil profile. Periglacial cover beds and loess sediments have been deposited on top of the bedrock.
2. During the second phase of slope formation, a first landslide occurs. In the course of the process, the permeable loess deposits slide on the top of the basal periglacial cover bed, which mainly consist of impermeable clay and marl (Damm and Terhorst, 2009).

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