가장 멋진 동굴 20곳

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

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Beautiful walk-in cave from quartzite mining

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Was on the way today.

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Orifice Alter/Tiefer Fürstenstollen Kunstgraben Roter Graben In the valley of the Freiberger Mulde, the mouth of the most important and longest Freiberger adit was attached to the main adit Stehenden. In the valley of the Freiberger Mulde, the mouth of the most important and longest Freiberger adit was attached to the main adit Stehenden. This tunnel, which was bought free by the Saxon sovereign in the late Middle Ages, was later called the Fürstenstolln. The mouth of the old/deep prince's adit has walls that can be dated to the 18th century. The mouth hole itself is part of a dry set wing wall. Above the vertical joints is a basket arch, including a coat of arms stone with the Saxon coat of arms. In the mouth hole there is a large sandstone tablet on the left joint, which marks the area zero for the area profile plan of the Freiberg area that was made in 1850-1852 and added later.

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Geological exploration and legend station If you hike along the Triebisch through the Tharandter Forest, you will come across not only the small ponds but also a cave on a slope above the Jungfernteich. This was probably created by human hands. The cave consists of low-quartz porphyry. It is located above the biotope ponds on the Triebisch (Triebisch Lakes). https://www.erzgebirge-tourismus.de/

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Mouth hole of the main break of the old deep Fürstenstolln "The mouth of the main adit is about 40 m east of the previous one at 321.2 m above sea level. In the unusual structure, the bottom left of the water column comes to light in a segmented arch, while on the right, three steps lead to the actual mouth above it. The high basket arch is again made of gneiss and set off as a pilaster strip.Since the water flowed across the entire width, a platform made of crossbeams was installed inside so that you could drive down the tunnel.The mouth hole was renovated in 2003 because the pit weather was used for cooling of the district hospital in the corridor." - https://de.wikipedia.org/wiki/Alter_Tiefer_F%C3%BCrstenstolln#Mundl%C3%B6cher

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This tunnel replaced the old deep Fürstenstollen, which was excavated along the corridor, passing through numerous benches and ridge structures and constantly running the risk of collapsing or becoming blocked.

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Andreas Alnpeckscher or Weißtaubner Stolln: A tunnel - in the Saxon region mainly written in proper names and traditionally also Stolln - is an underground passage driven horizontally or slightly rising into a mountain or hill from the surface of the earth, which creates a connection to a pit . The main function consisted in the removal of accumulating groundwater and in order to supply fresh air into the mine. Most of the tunnel mouth holes can therefore be found in the immediate vicinity of rivers or streams. The mouth hole of the Alnpeckschen tunnel was set up near the bank of the Mulden and is on the other side of the fence on the premises of the explosives factory. The escaping tunnel water is still used today. The tunnel had drifted east into the mountains. Its course can still be followed safely at the numerous break-ins and heaps.

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Here, too, the information boards on the geological trail provide interesting information about the geological features.

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Part of the Freiberg dynamite hiking route. A great hike for those interested in mining

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locked old mining entrance

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