Verbreitung, Ursachen und Füllung glazial übertiefter Talabschnitte an Beispielen aus den Ostalpen

Dirk Van Husen
In the investigated area a relationship between the appearance of widespread glacially deepened basins and the extent of active glacier terminus could be found. Those lie in the ablation area of these and probably are due to the high velocity of flowing ice and its increasing heavy charge of morainic debris. At the beginning of Late Glacial Time the refill of the basins was very fast. It was already achieved at the time when the...