周辺の洞窟・トップ11

So now the cave is also barred.

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The old tunnels in the Hunsrück make the region an important habitat for various species of bats. Here you'll find one of these tunnels, which can be lit outside of hibernation times so you can take a look inside.

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Nice rock formation, looks real, like a bear hole, but small.

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Hopefully the lucky stone will always be there. He who seeks finds

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A small detour of 20m is always worthwhile for a photo.

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You could go in a little, after a few meters there was a grille. Head bumped when leaving the tunnel. So take care!

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The highlight is twofold.

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Roof slate The roofing slate deposits of the Hunsrück date back to the Lower Devonian period around 400 million years ago. They were formed from clayey marine deposits, which later solidified into layered claystones and were "slated" during the folding of the Rhenish Slate Mountains. Foliation is a consequence of the directed pressure in the earth's crust during mountain formation, during which the mineral components of the claystones align in parallel and partially reform. Roof slate is the name given to clay slate in which the layering of the claystone and the foliation run parallel. This makes it possible to split large and thin plates. The Hunsrück slate, which is characterized by its uniform gray-black color, weather resistance and easy splitting, is one of the best varieties of German roofing slate deposits.

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