Large landslides belong to the most dangerous natural hazards in alpine environments, where rock slopes rather collapse through multistage failures than in one single event. Also, water in the travel path may cause high impact waves and long runouts. In this dissertation, a complementary method application at Lake Oeschinen (Bernese Alps, Switzerland), Lake Eibsee (Bavarian Alps, Germany) and at the Flims rockslide (Grisons Alps, Switzerland), yields novel results for the reconstruction of rock-slope failure in space and time and their secondary effects when impacting a lake.
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Large landslides belong to the most dangerous natural hazards in alpine environments, where rock slopes rather collapse through multistage failures than in one single event. Also, water in the travel path may cause high impact waves and long runouts. In this dissertation, a complementary method application at Lake Oeschinen (Bernese Alps, Switzerland), Lake Eibsee (Bavarian Alps, Germany) and at the Flims rockslide (Grisons Alps, Switzerland), yields novel results for the reconstruction of rock-...
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