프라우엔슈타인‬에서 가장 멋진 ‪20‬개의 천연기념물

도르테네펠젠은 클링겐베르크 저수지의 동쪽 기슭에 위치한 오르토그나이스로 이루어진 바위 돌출부입니다. 대부분 클링겐베르크 저수지의 가장자리는 완만하게 경사진 언덕으로 둘러싸여 있습니다. 하지만 한 지점에는 길 바로 옆에 큰 바위 돌출부가 있습니다. 작은 표지판이 등산객에게 이곳이 도르테네펠젠이라고 알려줍니다. 전설에 따르면, 목재 제재소의 아름다운 뮐러의 딸이 이곳에서 연인과 만났다고 합니다. 오래된 제재소는 이제 저수지의 물에 잠겼지만, 바위는 여전히 서 있고 그 발치에는 벤치가 놓여 있습니다. 원하는 사람은 위로 올라갈 수도 있습니다(주의, 길이 없음). 저수지의 아름다운 전망을 즐길 수 있습니다.

always worth a trip

Geographical Center of Saxony. Information: This marker, a granite stele in front of the Diebskammerfelsen (Thieves' Chamber Rock), was erected because the official geographical center (not far from here) was only developed for tourism in 1995.

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.

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.

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.

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.

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/