Die pleistozänen Schotter und Moränen zwischen oberem Mindel- und Wertachtal (Bayerisch—Schwaben)

Konrad Rögner
Pointers of a Donau-piedmont glaciation could be found also in the region between the upper Mindel and the Wertach valley. The western ice lobe of the pleistocene Lech-glacier has advanced the region of Kaufbeuren during the Donau-glaciation. This fact is documented by the presence of moraine deposits at Bickenried. The Donau-moraine and the correlating gravel body are intertonguing between Bickenried and Irsee. The age of the Donau-glacial sediments could be concluded from their stratigraphic relations...