Die plio- und pleistozänen Schotter der Wutach-Donau am Ost-Schwarzwald

Willi Paul
The gravels of the "Wutach-Terrace", final sediment of the river before its running over to the Rhine and until now supposed to represent stratigraphically the Lower Terrace as a sedimentary unit, are composed of t w o gravel beds separated the one from the other by a distinct discordance, here and there as-it seems — even by warm time sediments with a notable discordance. Moreover both gravel beds show a different degree of conservation. The...