Hazard warning area Susceptibility to slipping

In areas prone to slipping, there is an increased susceptibility to the formation of a deep slipping process. Deep landslides are downhill movements of rocks or loose rocks. The speeds of the sliding masses range from a few centimeters per year to several meters per minute.
Further information on the interpretation and the procedure for the preparation of the hazard warning card can be found in the reports on the hazard warning cards: https://www.lfu.bayern.de/geology/mass movements_maps_data/hazard maps/index.htm