Top 11 Caves ノイハウゼンでの

Old video of the "mine"! https://youtu.be/0HAQ8IZwJjA

Promisingly, it's advertised with a large sign. Sorry, but a cave doesn't look like much. Perhaps a fox could live in here. But it's not really an attraction. Access would have to be cleared first.

The cave is accessible via a hiking trail and has a small access hole. For those who aren't experienced cavers and have the appropriate equipment, there's a beautiful rock formation at the entrance.

Fluorite and barite were mined at the Käfersteige mine until 1997. The Käfersteige area is believed to contain the largest fluorite deposit in Europe. The former tracks that led into the tunnel can still be seen at the former Käfersteige tunnel entrance. The video-monitored access to the tunnel is closed and cannot be entered.

It's hard to believe. It's almost on the road, but not visible from it. A grotto-like sandstone rock formation with a central bench.

From the outside, only small holes are visible; the entrances have largely been covered with leaves and earth over the centuries. The air currents from the interior of the cave, however, suggest that an extensive cave system lies behind it. The cave is the second largest around Bad Liebenzell, after the Walzquelle spring.

The Beutelstein is located directly at the bottom of the Nagold valley near Bad Liebenzell. The top layer of the Bunter sandstone extends to the valley floor here. The basement rock of gneiss and granite is located beneath the Bunter sandstone. The Nagold has not dug deep enough near Bad Liebenzell to expose the basement rock. However, south of Bad Liebenzell there is a place where the Forbach granite is exposed on a road embankment. The boundary between granite and Bunter sandstone is therefore somewhat higher there than directly near Bad Liebenzell.

The Beutelstein is located directly at the bottom of the Nagold valley near Bad Liebenzell. The top layer of the Bunter sandstone extends to the valley floor here. The basement rock of gneiss and granite is located beneath the Bunter sandstone. The Nagold has not dug deep enough near Bad Liebenzell to expose the basement rock. However, south of Bad Liebenzell there is a place where the Forbach granite is exposed on a road embankment. The boundary between granite and Bunter sandstone is therefore somewhat higher there than directly near Bad Liebenzell.