File:Albtrauf NSG-Rutschen Kalktuff-Hochwiese Schwaebische-Alb.jpg
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Deutsch: Das Blockbild zeigt die Hochfläche, die Abrisskante und spezielle Hangeigenschaften eines Seitentals der Schwäbischen Alb nordwestlich von Bad Urach. Wie an vielen Steilkanten der Alb zum Albtrauf entspringen aus dem so genannten „Seichten Karst“ über nicht-verkarsteten oder stauenden Schichten Karstquellen, deren Wasser allmählich Klingen, Kerbtäler oder breite Täler erodiert haben. Im Naturschutzgebiet „Rutschen“ (Hochfläche und Traufkanten des Ermstals und Runden Berg) haben Karstquellen zwei unterschiedlich große Kalktuffterrassen, so genannte „Hochwiesen“ geschaffen. An deren steilen Abrisskanten haben sich der 37 m große, freie Uracher Wasserfall und die Gütersteiner Kalktuffnasen gebildet. Graphik verändert mit Daten von Georg Wagner, 1960. English: The pictorial schematic shows the plateau, the scarped ridge and special conditions of the slope of a side valley of the Swabian Alb, northwest of Bad Urach. As in many cases of the “Alb’s escarpment the karst springs emerge over impermeable rock layers, where the water eroded Klingen or V-shaped valleys with small or larger floodplains. In the Naturschutzgebiet “Rutschen” (Runder Berg and protection of the plateau and the scarped ridges along river ”Erms”) karst spring water sedimented two large calcareous tuff terraces, called “High Meadows”. Over these terraces’ scarped ridges “Uracher Wasserfall” and Gütersteiner Kalktuffnasen” shed their water. |
| Date | |
| Source | Own work |
| Author | Ustill |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 12:26, 10 August 2016 | | 1,800 × 613 (505 KB) | Ustill (talk | contribs) | User created page with UploadWizard |
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