Fig. 4From: Distribution, geometry, age and origin of overdeepened valleys and basins in the Alps and their forelandLongitudinal cross-section of the Traun Valley showing glacial tongue basins finally shaped during the LGM (Traunsee) and during the Lateglacial Gschnitz Stadial (Hallstätter See). Both lakes are presently being filled by delta sediments of the River Traun (modified after van Husen 1979)Back to article page