하르트만스도르프-라이헤나우‬에서 가장 멋진 ‪20‬개의 산 정상

In 2022, two Lichtenberg natives, Jörg and Sven, had a special idea: they wanted to revive an old local legend – the legend of the "Light on the Mountain." This tale, passed down from generation to generation for centuries, was deeply intertwined with the history of Lichtenberg and its surroundings. Inspired by this somber legend, Jörg and Sven decided to create a symbol of hope and light. They planned to erect a new summit cross on the mountain that would glow at night, just like the light in the windows of the old legend. But this light would no longer spread fear, but rather inspire hope. Two chimes are also mounted in the center of the cross, which, played by the wind, carry peaceful sounds down into the valley. Opposite the cross is a new selfie stand, perfect for taking a selfie.

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.

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.

Mountain peaks and stamp stations for the 14x 8000m peaks, there are well-made information boards for the Blockline here.

The Hemmschuh is one of the eight-thousanders in the Ore Mountains. You must bring an ink pad or a pencil for the stamp station.

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.

A great view and a good snack.

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.