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An evapo-transpiration controlled landslide in Switzerland: The Steinernase case

Between Zürich and Basel the highway passes close to Germany only separated by the Rhine River. At this point the main road and the railway have to pass the slope dipping toward the Rhine. This whole slope is creeping with faster sliding parts attending velocities up to 6 cm per year respectively 4 cm per month during crises. The slope is located in the forest, dipping 25 ◦ northwards and lies between 510 and 280 m a.s.l. The biggest sliding area in this slope covers about 130’000 m2 from which 30’000 m2 are sliding faster. It is a translational slide with a sliding surface at a depth of 3 (top of the slide) to 20 meters (on the slide base). Because of several slope stability problems during building of the roads and the railroad, the slide has been studied since 1911. Due to this much data is available.