File:Guetersteiner Wasserfall.jpg

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Deutsch: Ausschnitt des Gütersteiner Wasserfalls am Albtrauf in der Nähe von Bad Urach.
Der Quellhorizont der 4 Schichtquellen befindet sich in der Karstschicht „Untere Felsenkalke (Kimmeridgium, ki2)" im oberen Hangdrittel. Das bloße Durchnässen der Flächen und die Moos-Assimilation aus dem Karstwasser begünstigen die chemische Ausfällung und Ablagerung von Calciumcarbonat am meisten. Der Kohlendioxid-Verbrauch der Moose steigert die Ausfällung enorm.
English: Detail of the Gütersteiner Wasserfall at the Albtrauf near Bad Urach, southern Germany.
Water percolates from behind 4 springs in the karst stratumKimmeridgian", high above the valley’s bottom. A maximal water surface and the Moss’ photosynthesis accelerate best the chemical precipitation of calcium carbonate from the water.
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current19:32, 1 February 2008Thumbnail for version as of 19:32, 1 February 20081,200 × 1,800 (2.93 MB)Ustill (talk | contribs){{Information| |Description= {{de|Ausschnitt des Gütersteiner Wasserfalls am Albtrauf in der Nähe von Bad Urach.<br> Der Quellhorizont der 4 Schichtquellen befinde

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