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
السجل المحدّث
https://espeleoworld.com/ar/c/hoehlen-am-suedwesthang-des-kittenberges-marsberg
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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.
الوصف
الشكل
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".
المياه
The softening was presumably caused by hydrothermal solutions that migrated along faults.
تفاصيل أخرى
In earlier times the rocks were used locally as scouring sand. The caves lie in the "NSG Kittenberg".
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الكهوف القريبة
المصدر: Geotopkataster Nordrhein-Westfalen (Geologischer Dienst NRW) (ogc-api.nrw.de)، مع تعديلات. 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 · بيانات عام 2026