Fig. 3From: Distribution, geometry, age and origin of overdeepened valleys and basins in the Alps and their forelandLongitudinal cross-section of the Salzach Basin near Salzburg showing the internal structure of a typical glacial tongue basin (modified after van Husen 1979). The River Salzach and its local tributaries (Königsee Ache, Taugelbach, Lammer) are responsible for coarse input into the basinBack to article page