File:Trockental Lone-Setzingen Schwaebische-Alb.jpg

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Deutsch: Trockental der Lone, Schwäbische Ostalb. An dieser Stelle, hinter der Mündung des Hungerbrunnentals (ebenfalls ein Trockental) bei Setzingen floss in einem regenreichen April wieder ein kleines Rinnsal bis zur nächsten Versickerung vor dem Ort Lontal. Die für das Rinnsal viel zu große Talbreite ist das Ergebnis fluvialer Ausräumung durch die wasserreiche, jungtertiäre Urlone, die hier floss, bevor sie durch die stärkere rückschreitende Erosion von Rheintributaren (Neckar, Fils) und zusätzlich durch die stetige Anhebung und Schrägstellung der Schwäbischen Alb spätestens zur Riß-Eiszeit geköpft wurde. Im gesamten heutigen Lonetal kann man sehen, wie ein Fluss durch Verkarstung nach und nach von der Oberfläche verschwindet.

English: dry valley of river Lone, Swabian Alb. In a rainy April this section of the perennial dry valley near Setzingen had surface water again. The premival Lone (Urlone), reaching back to Lower Miocene and maybe earlier is one of the oldest rivers of Southwest Germany. Yet faster headward erosion of Rhine tributaries and tectonic uplift of the Swabian Alb’s northern escarpment finally captured the Urlone. Throughout the valley of the Alb’s residual Lone one can observe how karstification lets a rivulet slowly fade away.
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current11:08, 19 May 2015Thumbnail for version as of 11:08, 19 May 20151,800 × 1,200 (2.59 MB)Ustill (talk | contribs)User created page with UploadWizard

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