Relief- und Talgeschichte des Randen-Berglandes (Kt. Schaffhausen und badische Grenzgebiete zwischen Schwarzwald und Hegau)

René Hantke
The drainage in the Randen area has changed several times since the Miocene. The Wutach and Aitrach valleys are witnesses of a former Aar river flowing into the Danube. During cold periods, the neighbourhood of Rhine and Black Forest ice supported the formation of ice caps of the Randen plateau and on slopes exposed to the NW, N and NE. In the Rissian, small tongues reached Bargen, the northernmost village of Switzerland. Their meltwaters, together...