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File:Massenkalkfelsen Veringenstadt Schwäbische Alb.JPG

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Deutsch: Felssporne am SW Ausgang von Veringenstadt, Schwäbische Alb.
Tektonisch bedingte Zerklüftung (Vergitterung von zwei Gräben) und fluviatile Erosion im s-förmigen Lauchert-Durchbruch haben die Massenkalkfelsen stark geformt.
English: Massive limestone rocks, not totally eroded by river Lauchert, Veringenstadt Swabian Alb. The irregular outcrop and the many fractures and joints are also a result of the increased regional tectonics, as two grabens intersected here.
Date Febr. 29th September, 2011
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Author Ustill
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current22:17, 7 February 2013Thumbnail for version as of 22:17, 7 February 20131,787 × 1,800 (4.34 MB)Ustill (talk | contribs)User created page with UploadWizard

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