File:Starzel-Schlucht Junginger-Giess Braunjura Vorland-Schwaebische-Alb.jpg

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Deutsch: Starzel-Schlucht nach Eintritt in eine weiche Braunjuraschicht (Dogger, Opalinuston). Im Hintergrund der Wasserfall "Junginger Gieß" bei Schlatt, Vorland der Schwäbischen Alb. Am Wasserfall ist eine Verwerfung dokumentiert, durch die die „Opalinustonschicht“, die auch als „Wasserfallschicht“ bekannt ist, nach oben gelangte. Die Starzel entsteht unmittelbar am Albtrauf und fließt, mäandernd, auf den selbst geschaffenen Bachablagerungen bis nach Hechingen durch das „Killertal“ und mündet schließlich in Bieringen in den Neckar.
Das kleine Flüsschen durchquert vom Weißen Jura bis zum Muschelkalk sämtliche Schichten des Jura und etwa zwei Drittel der Trias. Der Bach begann als kleiner Nebenarm des Neckars und schnitt sich mit stetiger „Rückschreitender Flusserosion immer weiter in die Schichtstufen des Vorlandes und schließlich elf Kilometer weit in die Hochfläche der Schwäbischen Alb ein.

English: Gorge of the Starzel (Neckar), after entering the Lower Aalenian, a stratum of the Brown Jurassic, Swabian Alb. In the back: the waterfall “Junginger Gieß”. As result of a “listric fault” the upper part of the “Lower-Aalenian” is exposed and water flow of the Starzel eroded 6 meters. The small Starzel meanders meanwhile from the plateau of the Swabian Alb (for ca. 13 km) through the northern Alb Foreland way down to river Neckar. This happened basically by Headward Erosion.
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Author Ustill

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current17:00, 20 August 2020Thumbnail for version as of 17:00, 20 August 20201,800 × 1,200 (3.09 MB)Ustill (talk | contribs)Uploaded own work with UploadWizard

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