베르츠도르프-회르니츠 주변 최고의 워킹 & 하이킹 경로

nice bar, invites you to linger 👍🏼

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good description of what he once served

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the path was overgrown so we gave up 👎🏼

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easily accessible and cute 👍🏼

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Steep climb, magnificent view from the tower. If the lodge is open, be sure to stop by 👍🏼 very nice hostess.

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Bridge to the view over the mountain snack bar. When the snack bar is closed, a dog patrols the area below.

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beautifully maintained Schlosshotel AltHörnitz

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The pump track facility at Lake Olbersdorf will be closed for an expected three months starting April 8, 2025. The reason for the closure is necessary repair work on the green areas surrounding the track. Damaged green areas will be restored and erosion protection will be improved. The goal is to permanently ensure the attractiveness and safety of the facility.

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An information board is located on the right side of the entrance to the church.

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There is also an information board here.

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An information board is located to the right of the entrance.

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The north bank invites you to linger. The area is spacious, beautifully designed and mining technology, such as information boards about the former open-cast mine, shows that it is not that long ago.

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The Roschertal owes its existence to a geological peculiarity. It is a breakthrough valley of the Mandau, which has cut through a basalt layer and underlying tertiary tuff layers. Such valleys are formed when a river erodes rock over long periods of time, while the surrounding area may rise or the water cuts deeper. Geological development: 1. Tertiary deposits: In the Tertiary period (around 65 to 2.6 million years ago) the area was characterized by volcanic activity. Tuff - a rock made of volcanic ash - was deposited. Later, basalt flows poured over it and formed a resistant covering layer. 2. Cutting of the Mandau: The Mandau, a tributary of the Neisse, began to work its way through the harder basalt layer over time. Since basalt is much more resistant than the tuff underneath, the erosion process was uneven. The softer rock layers were eroded more quickly, so that the valley gradually deepened. 3. Formation of the breakthrough valley: As the rock was further eroded, the steep, wooded slopes of the Roschertal that are visible today were created. These reach heights of around 50 to 60 meters above the valley floor. 4. Late Pleistocene influence: During the ice ages, the landscape was further shaped when frost weathering and landslides affected the valley flanks. During this time, the Mandau transported more meltwater and debris, which caused the river to dig in further. Special features today: The Roschertal is not only a geologically interesting area, but also an example of the natural development of Upper Lusatia. The interplay of basalt and tuff layers gives the landscape a varied morphology. Erosion has created some bizarre rock formations, and the forest that has developed in the valley protects the loose rock layers from further erosion. The fact that the Mandau has formed a breakthrough valley here also influences the water dynamics. The flow can vary greatly depending on the water level, which is noticeable in small cascades and whirlpools. In summary, the Roschertal is a product of the volcanic past, fluvial erosion and ice age processes - an exciting geological formation that also offers an attractive landscape for hikers and nature lovers.

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The observation tower on the Breiteberg is a popular excursion destination near Zittau. The Breiteberg is about 510 m high and offers a fantastic panoramic view of the Zittau Mountains, the Lusatian Mountains and, when visibility is good, as far as the Jizera Mountains and the Giant Mountains. The stone observation tower was built in 1900 and is now a listed building. It is about 15 meters high and was built at the time to replace a wooden structure. Next to the tower there is a restaurant, the "Breiteberggaststätte", where you can stop for a bite to eat. The mountain is easily accessible via various hiking trails, e.g. from Großschönau, Hainewalde or Bertsdorf. A clear panoramic view awaits you at the top - perfect for nature lovers and photographers!

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The asphalted wave track is one of the medium-sized facilities of its kind in Saxony and is suitable for use with a wide variety of sports equipment such as bicycles, skateboards, scooters, etc. for all age groups.

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Only open when restaurants are open

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The Olbersdorfer Lake is located on the edge of the Zittau Mountains in eastern Saxony and is a popular local recreation area. The lake was created from a former brown coal open-cast mine, which was flooded after it was closed. Today it is a successful example of the renaturation of mining areas. Size: The Olbersdorfer Lake has a water surface of around 60 hectares. Depth: The maximum depth is around 36 meters. It is located in the immediate vicinity of Zittau and offers a wonderful view of the mountains of the Zittau Mountains.

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It is good that such memorial stones exist.

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Read the inscription and you will know more about it.

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It's a great place for hiking.

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