File:Urbrenz-Pleistozaen Goldshoefer-Sande Keuper-Feuersteine.jpg

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Deutsch: Gewässernetz einer pleistozänen Urbrenz. Die bis ins Hohenlohische reichenden Brenz-Zubringer waren ein breites, mit sehr geringem Gefälle fließendes Zopfstrom-Flusssystem. Erforschungen zu den Ablagerungen Goldshöfer Sande und zu Keuper-Feuersteinen, die in Steinbrüchen, Sandgruben und fluviatilen Höhenterrassen im Gebiet der Schwäbisch-Fränkischen Waldberge, in Ablagerungen vor und in der Albpforte bei Aalen gefunden wurden, haben zahlreiche Geoarchive erschlossen. Diese belegen hinreichend, dass die heutige rheinische Entwässerung der der östlichen Schwäbischen Alb nördlich vorgelagerten Schichtstufenlandschaft (hier: Schwäbisch-Fränkischen Waldberge), ursprünglich über die Schwäbische Alb zur Donau gerichtet war. Verändert nach Reiff&Simon 1990, Etzold 1994 und Strasser, A. 2009.

English: System of Pleistocene km-wide braided rivers, flowing with a very gentle gradient. Research on the not cemented sediments called "Goldshöfer Sande" and on Keuper-Flintstones, found in quarries and highest fluvial terraces of the Schwäbisch-Fränkische Waldberge and around Aalen’s river gate to the Swabian Alb verified that the contemporary rhenish drainage of the northeastern Schichtstufenland was all danubian across the Swabian Alb until it was captured in Middle Pleistocene.
Date March, 4th, 2015 (upload)
Source see author
Author Ustill

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