Figure 3:

View Original Image at Full Size

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).

Image 14954 is a 2169 by 1863 pixel JPEG
Uploaded: Apr9 09

The file is referred to in 1 page
Created by the author of the page containing
this file.
This item is offered under a Creative Commons Attribution-NonCommercial-ShareAlike license You may reuse this item for non-commercial purposes as long as you provide attribution and offer any derivative works under a similar license.