File:Hangschutt Karst-Quelle Schlattstall Schwaebische-Alb.jpg

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Deutsch: Hydrogeologisches Phänomen des „Seichten Karst“ in Schlattstall (Seitental von Lenningen), im tief eingeschnittenen Albtrauf der Mittleren Schwäbischen Alb. Die kleine Karstquelle, eine so genannte Schichtquelle, liegt hinter einem sehr steilen Hang des Mühlbergs verborgen, welcher zum relativ großen Naturschutzgebiet „Oberes Lenninger Tal mit Seitentälern“ gehört. Das wie ein Gleitmittel wirkende Karstwasser des nicht sichtbaren Quellaustritts hat den Hangschutt so unstabil gemacht, dass er über ca. 20 m samt der Hangvegetation bis zum Talboden abgerutscht ist. Der Hang schneidet eine wasserstauende Schicht an. An diesem Berghang treten an verschiedenen Stellen Karstwasser aus, u.a. aus den beiden großen Karstquellen „Schlattstaller Goldloch“ und Schwarze Lauter.

English: Small karst spring in the side valley “Schlattstall” where the valley deeply cuts the cuesta of the Swabian Alb (Albtrauf). The spring’s water, overflow of an impounding bedding, is hidden behind the mountain’s steep slope. The water worked like a slippery fluid, letting the debris and all vegetation slide down to the bottom. Only there, the water emerges.
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current16:41, 7 January 2017Thumbnail for version as of 16:41, 7 January 20171,200 × 1,800 (3.15 MB)Ustill (talk | contribs)User created page with UploadWizard

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