File:Lauchert-Giessfall Kalktuffbarre Veringendorf Schwäbische Alb.jpg

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English: waterfall of the Lauchert at Veringendorf, Swabian Alb.
6-8m packed fluvial sediments (tufa, travertine, Kalktuff (German)) of holocene age cover a 1,8 x 0,5km valley and abruptly end in a waterfall, called "Gieß Wasserfall".
Deutsch: "Gieß-Wasserfall" mit holozänem, fluviatilen Sediment der Lauchert vor Veringendorf, Schwäbische Alb.

Der Fluss füllte ein breites Tal von 1,8 x 0,5km. Im Bild ist rechts ist die Abrisskante (Kalktuffbarre) des bis zu 8m hohen, kompaktierten, aber sehr porösen, Kalktuffs zu sehen.

Das recht große Wasserbecken läßt erkennen, dass früher viel größere Wassermengen hinabstürzten. Die Mündung der "Ahlenbergquelle" mit der Quelle wenige Meter rechts hinter der Tanne, ist deutlich sichtbar. Die zweite Quelle, die so genannte "Wasserfallquelle", kommt unter dem Wasserfall hervor.
Date Jan. 2013 (upload)
Source see author
Author Ustill

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current18:24, 5 February 2013Thumbnail for version as of 18:24, 5 February 20131,800 × 1,200 (3.1 MB)Ustill (talk | contribs)User created page with UploadWizard

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