File:Teufelsklinge-Heubach Ostalb.jpg

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Deutsch: Teufelsklinge, Felswand und Quellöffnung. Die Erosion der intermittierenden Karstquelle am Albtrauf der Ostalb bei Heubach hat eine senkrechte, halbrunde Quellnische mit 100m Durchmesser und einer Höhe von ca. 80m geschaffen. Der vom Quellwasser gelöste Fels-Schutt und dessen Transport, die Quellwasser, einschließlich der Niederschlagswasser, haben in den Berghang eine Klinge (kleines Kerbtal) erodiert, ein Seitental bis zum Talboden. Vgl. Teufelsklinge Talblick
English: Teufelsklinge, mountain cliff and small v-shaped valley, eroded by Scree and water at the Albtrauf (cuesta) of the eastern Swabian Alb.
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current15:35, 2 August 2010Thumbnail for version as of 15:35, 2 August 20101,200 × 1,800 (2.15 MB)Ustill (talk | contribs){{Information |Description={{de|1={{de|Teufelsklinge, Felswand und Quellöffnung. Die Erosion der intermittierenden Karstquelle am Albtrauf der Ostalb bei Heubach hat eine senkrechte, halb

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