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마지막 업데이트: 4월 8, 2026
하이라이트 • 기념물
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하이라이트 • 자연 기념물
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프라우엔슈타인 주변 인기 장소
Flying high on two wheels – bike holidays in the Ore Mountains
전력 풀로 – 드레스덴 주변 철도 자전거 로
Wandertouren - Handwerk & Heimatgenuss
BLOCKLINE – Dein Bike-Abenteuer im Erzgebirge
BLOCKLINE-Gesamtstrecke in 5 Tagen – Bike-Urlaub im Erzgebirge
프라우엔슈타인 하이킹
프라우엔슈타인 로드 사이클링 경로
프라우엔슈타인 사이클링
프라우엔슈타인 주변 그래블 라이딩
프라우엔슈타인 러닝 트레일
The stream that has been dammed to form the alluvial ponds flows into the Mortelgrund at the Mortelmühle. Overall, the area with its bodies of water, riverbanks, mountain meadows and wet meadows represents a very valuable habitat.
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Beautiful place with a great view. The sea of stones at Stephanshöhe is a station on the 14x8000 and was probably also the devil's place of refuge, according to the story on the information board.
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Beautiful place with a great view. The sea of stones at Stephanshöhe is a station on the 14x8000 and was probably also the devil's place of refuge, according to the story on the information board.
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The Stephanshöhe is one of the eight-thousanders in the Ore Mountains. You will need to bring an ink pad or pencil with you to the stamp office. A bench invites you to take a break.
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Steinmeer at the Stephanshöhe The Steinmeer is located on the western edge of the approximately 15 km² Schellerhauer granite. In the period between Carboniferous and Permian, this rose as molten magma in the gneiss of the Erzgebirge basement and in the surrounding Teplice rhyolite and solidified below the earth's surface. Over time, the Schellerhauer granite was exposed by erosion. The penetration of the Schellerhauer and other granites in the Altenberg area was accompanied by a partial transformation of the adjacent rock. This also prevents the formation of numerous deposits, e.g. B. of tin and iron connected. The Teplice rhyolite here, which was heavily stressed by the geological processes mentioned, was gradually broken down to block and stone size, mainly by frost weathering. The Steinmeer on the Stephanshöhe is a witness to this process.
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The Dorotheenfelsen is a rocky outcrop on the eastern bank of the Klingenberg dam, which consists of orthogneiss. Gently rising slopes usually line the edges of the Klingenberg dam. But at one point there is a large ledge right on the path. A small sign tells the hiker that this is the Dorotheenfelsen. According to legend, the beautiful miller's daughter from the wood mill met her lover here. The old mill is now hidden by the water of the dam, the rock is still standing and at its foot you can sit on a bench. If you want, you can also climb up (caution, there is no path) and enjoy the beautiful view over the reservoir. - https://www.dresden-elbland.de/de/poi/geotop/dorotheenfelsen-klingenberg/60324250/
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