File:Trockental Wiesental-Sonnebuehl Schwaebische-Alb.jpg

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Deutsch: Das „Wiesental“ östlich Undingen, Mittlere Kuppenalb, ist ein kleines Trockental, welches unmittelbar vor der 1991 als Naturdenkmal geschützten Massenkalk-Kuppe „Kalkstein Südwest“ (erhaltenswerte Halbtrockenrasengesellschaften mit besonders geschützten Tier- und Pflanzenarten) in ein langes Trockental mündet, dessen Mittelteil auf topologischen Karten als „Großes Rinnental“ bezeichnet wird. Aufgrund der Topologie, der Höhenangaben und der von Thekla Abel 2003 nachgewiesenen alten Flussterrassen kann man einen plio-pleistozänen Fluss Ur-Erpf rekonstruieren, der vom Ruoffseck am Albtrauf bis zur Mündung in eine Urlauchert reichte. Das bis zu den aktuellen Quellen der Erpf (im Ort Erpfingen) reichende Trockental ist ca. 10,5 km lang. Demnach ist die wasserführende Erpf im Laufe ihrer Flussgeschichte auf ca. ein Fünftel ihrer ursprünglichen Länge geschrumpft.

English: Small dry valley "Wiesental", east of Undingen (Sonnenbühl), Middle Swabian Kuppenalb. The huge limestone mound in the back is a protected Naturdenkmal, "Kalkstein Südwest". The valley Wiesental flows into a 10,5 km long dry valley, of which the middle section is called "Großes Rinnental". Topology, elevation and old fluvial terraces, documented by Thekla Abel 2003, allow the reconstruction of a pliocene-pleistocene Ur-Erpf, which flowed into an de:Urlauchert. As the contemporary surface water Erpf is only 2,8 km, the rivulet obviously has a length of only one-fifth of its Ur-Erpf.
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current11:10, 19 May 2015Thumbnail for version as of 11:10, 19 May 20151,800 × 1,200 (2.38 MB)Ustill (talk | contribs)User created page with UploadWizard

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