Zur Paläogeographie der nördlichen Iller-Lech-Platte und zur Genese ihrer Schotter im Altpleistozän

Manfred Löscher, Klaus Münzing & Wolfgang Tillmanns
The existence of the Danube in the NW area of the Iller-Lech-Platte during the Lower Pleistocene which has been proven by gravel analysis leads to the conclusion that the Hier flowed in a NE direction until the Lower Pleistocene. The direction of the present drainage manifests for the first time with the sedimentation of the "Zwischenterrassenschotter". It is possible by means of heavy minerals to follow only a short distance the direction of the lower...