Wiehler Tropfsteinhöhle
The dripstone cave in a limestone quarry was formed by the dissolution of Devonian limestones and has been accessible as a natural monument since 1927.
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Wiehler Tropfsteinhöhle
The dripstone cave in a limestone quarry was formed by the dissolution of Devonian limestones and has been accessible as a natural monument since 1927.
Wiehl
最新资料
https://espeleoworld.com/zh/c/wiehler-tropfsteinhoehle-wiehl
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The dripstone cave in a limestone quarry was formed by the dissolution of Devonian limestones and has been accessible as a natural monument since 1927.
描述
形态
The total length is 1600 m, the depth 30 m.
洞穴次生沉积物
The cave contains dripstone formations, cascades and sinter curtains.
其他详情
The dripstone cave in a limestone quarry was formed by the dissolution of Devonian limestones (a lens-shaped limestone intercalation in the clayey Mühlenberg beds). The cave has been open to the public as a natural monument since 1927.
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附近洞穴
来源：Geotopkataster Nordrhein-Westfalen (Geologischer Dienst NRW)（ogc-api.nrw.de），已修改。 Data licence Germany – attribution – version 2.0 (dl-de/by-2-0), https://www.govdata.de/dl-de/by-2-0 Geowissenschaftliche Daten: INSP-GeotopeinNRW @ Geologischer Dienst NRW · 2026年数据 · 来源：Wikidata – cave items (Germany)（www.wikidata.org），已修改。 CC0 1.0, https://creativecommons.org/publicdomain/zero/1.0/ Wikidata (CC0 1.0) · 2026年数据