ウォルケンシュタインでののおすすめウォーキング＆ハイキングルート

Impressive rock face, tough climb and great narrow gorge

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signpost

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a very nice corner

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Walking through this fantastic landscape, we reach the Zschopau River and follow its course. Near the railway bridge, a rock formation blocks the path along the water. As we ascend and then descend again, the railway tracks now accompany us, which we cross shortly after. Here's our entire hike https://youtu.be/GoJzFTXM5iU

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Back on our path, a beautiful panorama awaits us, now between the meadows stretching across the hilly landscape and the old town with the castle in the background. After a moment, we enter the forest. Here's our full tour https://youtu.be/GoJzFTXM5iU

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The rock massif between Wolkenstein and Floßplatz, the "Wolkenstein Switzerland", is a great place for hiking with small scrambles and wonderful views, but there are also many opportunities for climbing here 🙃.

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A very nice corner

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The path through the Wolfsschlucht Gorge leads down to the river. This is also the starting point for the via ferratas.

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a very nice view

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Here begins the descent into the Wolfsschlucht and the access to the via ferratas.

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The path through the Wolfsschlucht leads down to the river. This is also where the via ferrata starts.

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Wolkenstein Castle is a high medieval castle that was first mentioned in documents in the 13th century. The town and castle stand on gneiss rocks 80 meters above the Zschopau valley. Wolkenstein owes its existence to the "Berggeschrei" (the cries of the mountain), that is, the discovery of the ore deposits. The settlement and ore mining is older than that of Annaberg-Buchholz.

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The deep valley with exposed gneiss is the result of the erosion of the Zschopau, which rises on the Fichtelberg and has been flowing in a northerly direction with a greater gradient since the uplift of the Ore Mountains block in the Tertiary period, and flows into the Freiberg Mulde near Döbeln. Steep, often bizarre rock faces are created on steep slopes by the increased flow speed. The most impressive formation is probably an overhanging cliff.

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The sign is located at the access point to the impressive bridge cliff.

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The deep valley with exposed gneiss is the result of the erosion of the Zschopau, which rises on the Fichtelberg and has been flowing in a northerly direction with a greater gradient since the uplift of the Ore Mountains block in the Tertiary period, and flows into the Freiberg Mulde near Döbeln. Steep, often bizarre rock faces are created on steep slopes by the increased flow speed. The most impressive formation is probably an overhanging cliff.

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When the forest is being swept (it was closed because of tree work) we have to take detours.

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great, always worth a trip. Very nice view

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View from below, view from above, ,--- here every view is special

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View of Selva

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Very close to the highlight, at the next intersection, there is also a great opportunity for a short rest with a view on some stones.

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