周辺の洞窟・トップ20

Information panel for the Andreas Alnpeck or Weißtaubner Adit, located on Heuweg. Information: The entrance to the Alnpeck Adit was located near the banks of the Mulde River and is situated beyond the fence on the grounds of the former explosives factory. Because the entire mining area was later leased to the Weiße Taube Mine (1695-1815), the Alnpeck Adit was renamed the Weißtaubner Adit.

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Info: Upper Triebisch Valley Geological Hiking Trail (GWOT). Heyneberg Limestone Mining. Panel 6: In the Lower Carboniferous, calcareous greywacke and limestone occur locally within the olisthous stream near Heyneberg. Between 1815 and 1831, the limestone marl from Helbigsdorf, among other places, was used to produce furnace slabs in the Freiberg silverworks. Geological Hiking Trail: The upper Triebisch Valley is known for the Upper Triebisch Valley Geological Hiking Trail (GWOT), which provides an insight into the geological history and geology of the region and is approximately 17 km long.

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According to legend, the shallow cave in the rock (quartz-armed porphyry or rhyolite) was once much larger, and three fairies lived there. On a full moon night, a minstrel who had previously played at the fair in Hintergersdorf (spa town of Hartha) passed by. The three fairies had laid out laundry on the meadow to bleach. The musician picked up a lace cloth and took it with him. However, when he got home, instead of the cloth, he held a gray cobweb in his hand. Before sunrise, he returned the cobweb to its place, where it became a lace cloth again, just as the other laundry disappeared with the first rays of sunlight. Since then, the fairies have not been seen again, and the cave has become a shallow hole.

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Located in a beautiful spot. Info: This was probably created by human hands. The cave is made of quartz-poor porphyry. According to legend, the shallow cave in the rock was once much larger, and three fairies lived there.

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Geological hiking trail Upper Triebischtal Panel 6

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On the lower slope is the "Heyneberg" limestone quarry with a rock face up to 12 m high old, small, south-facing quarry with excavation for lime extraction, south-east of Heyneberg. Height of the slate rock walls alternated with calcareous and quartzitic greywacke, max. 15 m.

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On the right side of the Röschenmundloch there is a small cave that was created by quartzite mining. Apparently, opportunity not only makes thieves but also miners, because this cave was created almost incidentally during the construction of the Rösche to extract quartzite for porcelain production.

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After a few hundred meters through the forest, a little off the Bobritzsch, the hiking trail and the artificial ditch, which is very well preserved here, reach the upper mouth of the 150-metre-long porcelain rock rose. On the right side of the Röschenmundloch there is a small cave that was created by quartzite mining. Apparently, opportunity not only makes thieves but also miners, because this cave was created almost incidentally during the construction of the Rösche to extract quartzite for porcelain production.

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