フラウエンシュタインの天然記念物・トップ20

ドロテエネフェルゼンは、クリンゲンベルク貯水池の東岸にある、正長石英岩でできた岩の露頭です。 ほとんどの場合、クリンゲンベルク貯水池の縁には緩やかに傾斜した丘が連なっています。しかし、ある地点では、道筋のすぐそばに大きな岩の露頭があります。小さな標識がハイカーに、ここがドロテエネフェルゼンであることを告げています。伝説によると、ホルツミュール（木材製材所）の美しい製材屋の娘がここで恋人と会ったと言われています。古い製材所は今や貯水池の水に隠されていますが、岩は今も立っており、その足元にはベンチに座ることができます。希望者は、上に登ることもできます（注意、道はありません）。貯水池の素晴らしい景色を楽しむことができます。

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/