Subnivale Kleinoserbildung. - Eine Beobachtung zur Schuttumlagerungsdynamik im Wimbachgries (Berchtesgadener Alpen)

Thomas Schneider
Mass transport on the vast dolomite debris surface of the "Wimbachgries" has vastly been attributed to summer thunder showers, with amounts of precipitation which cannot immediately be swallowed by the large detrital valley filling, thus leading to torrential rock How processes. However, spring snow melt regularly exposes accumulative forms which indicate that subniveal or intraniveal debris transport must have taken place. Due to a striking resemblance to their macro equivalents, these forms are called subniveal...