Eine saaleeiszeitliche Mittelmoräne zwischen Teutoburger Wald und Wiehengebirge

Ernst Th. Seraphim
The author gives the first description of a middle-moraine of the Saalian glaciation in northwestern Germany. The formation of it is a consequence of the relief, especially of the passages in the Wiehen-Mountains, which influenced the inland ice gaining ground from the north towards the Herford Lias depression.