File:NSG-Ammertal Muschelkalk-Steinbruch Reusten.jpg

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Deutsch: Oberer Muschelkalk in einem aufgelassen, bis ins Grundwasser reichenden Steinbruch des Naturschutzgebietes Kochhartgraben und Ammertalhänge, Kreis Tübingen. Über dem südexponierten Steilhang liegt eine landwirtschaftlich bedeutende, flache Lettenkeuperdecke. Die Steilwand zeigt im mittleren Bereich die Schichten der Nodosuskalke, (Teil der Meißner-Formation Ceratitenschichten). Diese oft dünnbankigen, tonig-plattigen, Schichten sind gegenüber den anderen Schichten relativ deutlich abgegrenzt. Oberhalb davon folgen Schichten der Trigonodus-Dolomite, deren Bankung undeutlich ist. Wie im Bild an mehreren Stellen sichtbar, neigen diese Schichten zu Mergeln zu verwittern. Über dem Hartgestein der Steilwand liegt ein typischer, flachgründiger Rendzina-Boden, dessen Feinerde stark kalkhaltig ist.

English: Outcropped Upper Muschelkalk (part oft he Middle Triassic) in a huge abandoned quarry, which reaches down into groundwater level. The quarry is part of a Naturschutzgebiet near Tübingen. The section in the middle of the vertical Upper Muschelkalk wall, having a clear lower and upper border, consists of thinly bedded limestone in which Ceratites are found. The beds above these are “Trigonodus dolomites” of which the bedding is kind of weak. As seen in several parts, these facies tend to weather into marls. The soil on top of the rocks is a thin layer of Rendzina.
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Author Ustill

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