Höhlen am Südwesthang des Kittenberges
The caves on the Kittenberg near Canstein formed through the softening of dolomitized Werra marginal carbonate of the Zechstein, presumably by hydrothermal solutions along faults.
EspeleoWorld
Höhlen am Südwesthang des Kittenberges
The caves on the Kittenberg near Canstein formed through the softening of dolomitized Werra marginal carbonate of the Zechstein, presumably by hydrothermal solutions along faults.
Marsberg
最新资料
https://espeleoworld.com/zh/c/hoehlen-am-suedwesthang-des-kittenberges-marsberg
信息可能会变化。出发前请务必核对坐标、通行情况、天气和洞穴状况。
The caves on the Kittenberg near Canstein formed through the softening of dolomitized Werra marginal carbonate of the Zechstein, presumably by hydrothermal solutions along faults.
描述
形态
The caves on the Kittenberg near Canstein formed through partial softening of dolomitized Werra marginal carbonate of the Zechstein. The grain fabric was completely destroyed in the process, so that the rocks disintegrated into "dolomite sand/ash".
水文
The softening was presumably caused by hydrothermal solutions that migrated along faults.
其他详情
In earlier times the rocks were used locally as scouring sand. The caves lie in the "NSG Kittenberg".
用户评论 (0)
暂无评论。
成为第一个分享体验的人！
已记录的探索 (0)
暂无探索记录。
记录您对这个洞穴的访问！
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