File:Kohlenkalk (gefaltet, Göhltal).jpg

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Deutsch: Die Wand befindet sich etwa östlich der Göhl und etwas südlich des Ortes Bleiberg (Plombieres) in Belgien.

Man sieht stark gefaltete Steine, sogenannten Kohlenkalk. Die Ablagerung erfolgte in der Zeit des frühen Karbon. Die starke Faltung war das Ergebnis der variszischen Gebirgsbildung (Orogenese) während der Zeit des Karbon.
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Author Rhetos

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current18:52, 19 August 2023Thumbnail for version as of 18:52, 19 August 20232,992 × 2,992 (3.63 MB)Rhetos (talk | contribs)Uploaded own work with UploadWizard

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