| Name: The Hunsrück Slate Location: Western Germany Age: Devonian |
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The Hunsrück slate (Hunsrückschiefer) occurs in a NW-SE trending belt 150km long by 15km wide. This belt is situated mainly south of the River Mosel and west of the Rhine in western Germany.
The Rhine and its tributaries have exposed the slate layers allowing access to the deposits. Most of the famous fossils have been discovered in the Bundenbach area.