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About: Dactyliocerassandstein Formation     Goto   Sponge   NotDistinct   Permalink

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The Dactyliocerassandstein Formation (also known as Epsilonkalksandstein Formation) is a Lower Jurassic (Lower Toarcian) geologic formation primarily located in Bavaria, Germany. The Formation appears on places like Bruck in der Oberpfalz, the north-east of the Banz Abbey, Wittelshofen, Regensburg and Bodenwöhr. In the astly foreland it extends from the Kulmbach area via Bayreuth, Creussen, Hirschau and Amberg to Schwandorf. Its southernmost known occurrences seems to be Schwandorf himself and Haselbach, although is also found at , far at the south. Is composed mostly by clusters of clay sandstone and sand-lime stone facies (shale, slightly bituminous in layers, and sandstone, lias sand, sand marl, marl, oolithic limestone and sand-lime banks) occurs only in the south-east of the northern