File:Kalktuff Gosbach Drackenstein Schwaebische Alb.jpg

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Deutsch: Kleiner Wasserfall mit großflächig bemoosten Kalktuffablagerungen, Gosbach, ein Bach in einem Seitental der Fils, Unter-Drackenstein, Schwäbische Alb. Diese Ablagerungen sind die Fortsetzung einer bis zu 150 m breiten und 20 m mächtigen Terrasse aus Kalktuffsediment. Oberhalb des Teilortes Unterdrackenstein befindet sich die Karstquelle des Gosbaches, dessen Wasser im steilen Hang das Kalk-Sediment chemisch ausfällte.
Auf dieser in den letzten Jahrtausenden seit dem Atlantikum (Quartärzeit) sedimentierten Kalktuff-Verebnung kauern sich 20 Häuser, dominiert von Kirche und Pfarrhaus des Dorfes. In den Kalktuffablagerungen befinden sich, wie geologisch vielfach zu beobachten, mehrere „Primärhöhlen“, darunter die ca. fünf m in die Ablagerung hineinreichende „Mariengrotte“, die, zusammen mit der Kirche, Weihestätte wurde.

English: Waterfall of stream “Gosbach”, heavily covered by mossy travertine, Unter-Drackenstein, Swabian Alb. The travertine sediment is the continuation of a 150 m broad and 20 m thick travertine terrace, accumulated by the karst spring’s water, which rises high above Unter-Drackenstein in a steep slope.
The terrace has 20 houses, the dominating church and the clergy house. As common in large travertine-sediments, there are primary caves in the sediment, including the “Mariengrotte”. This and the church used to attract as catholic sacraments.
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