File:Fluss-Anzapfung Strunkpass Schwäbische Alb.jpg
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English: Geological cross section NW-SE: Swabian Jura: Forland at Rottenburg, Alb-Cuesta at Talheim and Mägerkingen on the Alb plateau.
Evidence of both, old fluvial terraces of river Neckar and fossils in Upper Danube-related former river-cave "Bärenhöhle (German)" were rated to be of "Tegelen" age (lower Pleistocene). The immense headward erosion of Neckar tributaries has captured Danube tributaries and created wind gaps. Karst phenomena accelarated the process. Deutsch: Geologischer NW-SE-Schnitt: Albvorland bei Rottenburg, Albtrauf bei Talheim und Kuppenalb bei Mägerkingen. Terrassenschotter am Rottenburger Neckar und einige Fossilien in der Bären- und Karlshöhle auf der Kuppenalb (deren Zugehörigkeit zu einer alten Lauchert erwiesen ist) konnten jeweils auf das Tegelen (Altpleistozän, 0,8 bis 1,8Ma) datiert werden. Starkes Gefälle (durch rückschreitende Erosion) der Neckartributare hat die Donautributare auf der Kuppenalb "geköpft". Die Karst-Morphologie im Quellbereich von Fehla und Lauchert zeigt breite Trockentäler, die "in der Luft ausstreichen", das sind offensichtlich Strunkpässe. Gezeichnet basierend auf Daten von "Ufrecht, W., plombiertes Höhlenstadium..." 2006 und topographische Karten 1:25000, Landesvermessungsamt BW, Stuttgart. |
| Date | Febr. 2013 (upload) |
| Source | see author |
| Author | Ustill |
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| current | 22:28, 8 February 2013 | | 1,800 × 1,200 (666 KB) | Ustill (talk | contribs) | User created page with UploadWizard |
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