Die interglazialen Kalksinterbildungen bei Hurlach nördlich Landsberg am Lech

Hermann Jerz & Joachim Mangelsdorf
On the western bank of the Lech river near Hurlach there are calcareous freshwater sediments with a great variety of features. The sinterformations are associated with organic layers and they contain a rich molluscan fauna (see Kovanda, in this vol.). According to the geological situation and from further investigations (palynology, malacology, U-Th-dating) it can be concluded that they are interglacial (Riß/Würm). The calcareous deposits are now isolated from the springs on the eastern slope of...