Die Älteren Schotter am Schwarzwaldwestrand, ihre Verbreitung, Genese und stratigraphische Stellung

Gaby Zollinger
The older gravel is distributed at the pediment of the western slope of the Black Forest lying under a loess-loam cover of the Würm period and were found as relicts between the valleys. It consists of fluvial sediments from periglacial debris and moraine which were deposited during the Riss Age. It is constantly eroded and redistributed by means of river systems of the Würm and Holocene Age. Since the early period of the Holocene, a...