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PORTAIL D'INFORMATION GÉOGRAPHIQUE

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  • Temporal occurrence of mass movements in the Bonn area
  • Geological and geomorphological patterns of the Bonn area are responsible for disposition for landsliding. The disposition was reinforced in the 19th century by mining activities, and in the 20th century by building houses on the slopes. Although
  • there is a strong human impact in the Bonn area, precipitation events are responsible for the temporal occurrence of landslides in the Bonn area, precipitation events are responsible for the temporal occurrence of landslides in the Bonn area. The amount of rainfall
  • 2001
  • , to classify different, climate-driven cycles of slope evolution and to identify potential risk areas. This study further shows that recent mass movements in Pleistocene landslides areas generally were triggered by subsurface and surface water. These results
  • 2001