File:Kalktuff-Stufen Karst Eschlipp Fraenkische-Schweiz Fraenkische-Alb.jpg

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Deutsch: Kalktufftreppe eines Karst-Baches zwischen „Eschlipp“ und Ebermannstadt, in der Fränkischen Schweiz, die zur verkarsteten Fränkischen Alb gehört. Der großflächige, bodennahe Pflanzenbestand ist der typisch lauchartig riechende Bärlauch, der in anhaltend feuchten, aber kalkreichen Humusböden junger oder ausgewachsener Kalkbuchenwälder schon im zeitigen Frühjahr den ganzen Waldboden bedeckt.

Der Karst-Bach verstärkt den in einem bewaldeten Seitental fließenden „Talbach“; in Ebermannstadt mündet dieser in die Wiesent (über die Regnitz zum Main). Durch reichlich Kalktuff gestufte Bäche gibt es mehrere in Karstgebieten Bayerns, Baden-Württembergs und in Kroatien ( Nationalpark Plitvicer Seen). In vielen Ländern der Erde mit verkarstungsfähigem Gestein sind Karstphänomene möglich.

(Verkarstungsfähiges Gestein Deutschland: Image:Karbonat-Aufschluesse Deutschland.jpg, Welt: Image:Carbonate-outcrops world.jpg)

English: travertinesteps of a karstic stream in Franconian Switzerland, (Franconian Alb, Bavaria). ransoms, widespread across most of Europe, here cover completely the floor of a young beech forest. Moist soils, slightly calcic, are favorable conditions. This and several other branches feed the stream “Talbach”, which joins the Wiesent at Ebermannstadt. There are several streams with travertine sediment in this formation in Bavaria, Baden-Württemberg and Croatia (Plitvice Lakes National Park). In the karstic world comparable phenomena are possible.
(Carbonate outcrop in Germany: Image:Karbonat-Aufschluesse Deutschland.jpg, World: Image:Carbonate-outcrops world.jpg)
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current09:45, 24 May 2017Thumbnail for version as of 09:45, 24 May 20171,800 × 1,200 (3.23 MB)Ustill (talk | contribs)User created page with UploadWizard

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