ヘルデッケの峡谷・トップ8
ヘルデッケには 8
の息を呑むほど美しい峡谷があります。以下に紹介する必見の峡谷一覧に掲載されている写真、おすすめ情報、その他のデータを参考にして、次の冒険でヘルデッケの美しい峡谷を訪れる際に役立てましょう。
最終更新日: 4月 11, 2026
ヴァンネバッハ渓谷
ハイライト • 峡谷
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ワンネバッハタール
ハイライト • 峡谷
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シュルマイスター採石場
ハイライト • 峡谷
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キュルプマン採石場の石の塔
ハイライト • 記念碑
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デュンネベッケ渓谷
ハイライト • 峡谷
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コミュニティからのヒント
The Dünnebecke Valley is very lovely. The narrow forest path led me along the edge of the beech forest, offering me charming views of the Wiesental valley.
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Historically interesting place on the way
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The Külpmann quarry is located on the Böllberg in Albringhausen, Wetter (Ruhr). Ruhr sandstone was mined in the quarry. The site was operated by the Külpmann family from 1932. The company filed for bankruptcy in 2012. Since 2013 there has been a sales warehouse for a natural stone dealer here. The quarry wall is a geological outcrop from the Carboniferous period that still exists today.
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The Külpmann quarry is located on the Böllberg in Albringhausen, Wetter (Ruhr). Ruhr sandstone was mined in the quarry. The site was operated by the Külpmann family from 1932. The company filed for bankruptcy in 2012. Since 2013 there has been a sales warehouse for a natural stone dealer here. The quarry wall is a geological outcrop from the Carboniferous period that still exists today.
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The quarry is currently inaccessible, but there is a viewpoint to the north that offers a view of the quarry. It is only accessible on foot via forest paths and is really worth it !!!
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The Neuwuelflingsburg colliery, which worked here until 1967, was formerly located on the quarry site. In addition to sandstone, layers of mudstone and a coal seam about 30 cm thick can also be seen in the quarry. The layers of rock belong to the Sprockhövel Formation and were deposited more than 300 million years ago. From time to time, the remains of tree trunks (lepidophytes) up to 2 m long are uncovered on fresh quarry walls as a result of quarrying. They are silent contemporary witnesses of a former forest moor landscape that existed during the Upper Carboniferous.
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Until a few years ago, Ruhr sandstone was mined in the Böllberg quarry to produce floor panels or facade panels, for example. The old factory building originally belonged to the Neuwuelflingsburg colliery, which worked here until 1967. In the walls of the quarry, primeval tree trunk remains up to 2m long were occasionally recovered during mining. They are remnants of a former forest bog landscape that existed during the Upper Carboniferous (320 to 296 million years before today).
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Above the old Külpmann quarry you have a wonderful (almost 360 degrees) view, among other things you can see as far as Wuppertal.
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