The South face of Dobratsch is a geomorphologically highly active zone, with frequent rock falls and occasional large landslides. Therefore, a lot of rocks and debris have accumulated at the base of the mountain, an area therefore known as "Schütt". In 1348, an earthquake-triggered landslide led to disastrous consequences.
- Location
- View on OpenStreetMap
- Created
- on Saturday 7 November 2020 by Martin Mergili
- Keywords
- cultural landscape, landslide, landslide deposit, lightscape, mountainscape, non-tropical montane forest, sedimentary rocks
- Visits and license
- 3602 visits, CC BY-NC-SA 4.0 DEED license