Die Goldshöfer Sande und die quartären Reliefgenerationen im Albvorland Ostwürttembergs

Reinhard Zeese
The objective is to correlate the sediments of Goldshöfe (Goldhöfer Sande) as river and talus deposits from the oldest Pleistocene with landforms and mechanism of erosion of the time of their deposition. Talus and fluvial deposits indicate an intermittent run-off. In less resistent rock also at the lower parts of slopes erosive periods of rill wash must have alternated with accumulative phases of "Spülsolifluktion" (rill wash solifluction). The landforms resulting from these mechanisms are wide...