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미셀베르그

가장 멋진 동굴 6곳

다음 모험 때 미셀베르그에 있는 동굴을 방문하고 싶나요? 그렇다면 미셀베르그에서 가장 멋진 동굴 9 개를 아래에서 살펴보세요. 다른 회원들이 경험을 바탕으로 추천한 콘텐츠인 만큼 믿을 수 있는 정보이니 마음에 드는 동굴이 있다면 다음 모험 계획에 추가해보세요.

마지막 업데이트: 2월 21, 2026

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하인첼만 동굴

하이라이트 • 동굴

They were created by chemically dissolving the limestone. Since such cave formations only take place in areas filled with groundwater, these processes must have occurred at a time when the …

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This tunnel previously served as an air raid shelter. Today it serves as a bat roost.
Inaccessible because it is locked with a thick iron door.

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최고의 싱글 트랙, 봉우리 및 다양한 흥미로운 야외 장소에 대한 추천을 받아보세요.

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오토-볼프-슈톨렌 박쥐 동굴

하이라이트 • 동굴

The Otto Wolff tunnel was started in 1935 to connect the Leopoldine-Louise mine to the Holzappeler mine. In civil engineering, the pit reached level 25 at 750 m below sea …

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Rullsbach와 Wiesbach 근처의 동굴

하이라이트 • 동굴

this head-high cave is located directly on the left side of the path between Rullsbach and Wiesbach!
The cave or the hole goes only a few meters into the rock …

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갱구

하이라이트 • 동굴

The Braubach lead and silver smelter, which today only scraps lead-acid batteries, has been an industrial monument since 2002.
Mining has been going on since 1691 to extract lead, tin, …

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무료로 가입하여 미셀베르그 주변의 더 많은 동굴을 발견하세요.

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uta_is_hiking

8월 20, 2023, Mundloch

The Braubach lead and silver smelter, which today only scraps lead-acid batteries, has been an industrial monument since 2002. Mining has been going on since 1691 to extract lead, tin, silver and other ores. The lead and silver works began operations in 1691. In the Rosenberg mine, mining took place in the Viktoria, Moritz, Segengottes and Gustav tunnels.

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The Otto Wolff tunnel was started in 1935 to connect the Leopoldine-Louise mine to the Holzappeler mine. In civil engineering, the pit reached level 25 at 750 m below sea level. The pit was accessed by at least 36 tunnels with a total length of 44 km (including vein sections) and by at least 17 open shafts and 8 blind shafts with a total depth of 4400 m. There were 25 levels down to a depth of 1067 m (= -789.2 m NN) Lots of information: https://de.wikipedia.org/wiki/Grube_Holzappel

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Here there is a short piece of rock face with many holes. Since they are the size of a head, they are ideal for “Heinzelmännchen”. The rock consists of karst and the small caves were created by erosion.

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The Heinzelmannshöhlen are located on the HöhenLuft hiking trail.

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Looks cool from the mountain

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Looks really cool 👍

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Interesting information board about the Otto Wolf tunnel

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This tunnel previously served as an air raid shelter. Today it serves as a bat roost. Inaccessible because it is locked with a thick iron door.

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The explanation board for the caves is at the top at the foot of the Concordia tower

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<< Heinzelmann Caves and Baedecker Felsenweg >> "The wildly romantic rock path high above Bad Ems along the rocks of the Bäderlei with ever new, magnificent views of the river landscape was already part of the standard tourist program for spa guests in the 19th century. On the way are the fascinating Heinzelmann caves. They are karst tubes, a strange one The whim of nature, around which countless legends are entwined. They were created by lime leaching. As early as the 18th century, they fascinated the natural scientist Senckenberg and Goethe's friend Lavater." https://www.daslahntal.de/info/infosystem/Heinzelmannshoehlen-und-Baedecker-Felsenweg_Bad/poi.html

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this head-high cave is located directly on the left side of the path between Rullsbach and Wiesbach! The cave or the hole goes only a few meters into the rock face, which is quite suitable as a shelter in bad weather!

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While there isn't much to see, it is definitely worth conserving. And has found another useful use for the bats.

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The Heinzelmannshöhlen was created by leaching limestone. Very interesting to look at ... 💥💥👍🥾

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Really strange to look at, was it nature?

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Till

11월 13, 2017, Heinzelmannshöhlen

The Heinzelmannshöhlen can be reached by a nice short ascent from Bad Ems. Continue up to the tower. Is part of one of the excellent walks in Bad Ems.

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They were created by chemically dissolving the limestone. Since such cave formations only take place in areas filled with groundwater, these processes must have occurred at a time when the Lahn and thus also the groundwater surface were above the level of the Heinzelmann Caves.

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되샤이트카우브바이젤캄프-본호펜장크트 고아하우젠오스터스파이오버발메나흐홀츠하우젠 안 데어 하이데브라우바흐발두인슈타인크램버그샤이트디에즈올스베르그필젠보르니히니더발메나흐리터샤인벨테로드닥센하우젠나스타텐오버나이젠랑겐샤이트비를렌바흐슈타인스버그구테나커로렌버그디타르트알텐디에즈케스터트Nassau립폰한슈타텐니더나이젠호르하우젠스트뤼트레테르트베른드로스레켄로스헤롤드클링겔바흐비브리히바젠바흐쾨르도르프브렘베르크카체넬른보겐홀자펠라우터트게일나우달하임플라흐트무더하우젠로하임이셀바흐에베르트하우젠라이커스하우젠프라트라이첸하인오베른호프되른베르크하이스텐바흐아텐하우젠에펜로드사우르탈바이내르나소함바흐패터스버그란슈타인베르그하우젠네츠바흐칼텐홀츠하우젠쉬에스하임보겔구킹겐노체른오버피쉬바흐니더티펜바흐에르게스하우젠Lierschied젬머리히샤를로텐베르크부르크슈발바흐아르츠바흐Winterwerb오버티펜바흐프뤼히트밀렌흄베르그미텔피쉬바흐아우엘오버바흐하임짐머쉬드베헬른슈바이그하우젠케메나우다우제나우웨이어니더바흐하임힘미호펜니에번켈바흐하이나우싱호펜카스도르프되르스도르프나쁜 Ems도른홀츠하우젠오버비스아이시고펜마리엔펠스가이식Fachbach디에네탈데시고펜엔드리히호펜롤쉬드밀렌베텐도르프에르훈젤

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