In areas prone to slippery, there is an increased susceptibility to the formation of a deep slipping process. Deep-reaching slides are downhill movements of rock or loose rock. The speeds of the slip masses move between a few centimeters a year up to several meters per minute. Further information on the interpretation and procedure for the preparation of the hazard statement card can be found in the reports on the hazard statement cards: https://www.lfu.bayern.de/geologie/massenbewegungen_karten_daten/gefahrenhinweiskarten/index.htm
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