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Schrattenkalk Formation

Aptian StageBarremian StageCretaceous AustriaCretaceous GermanyCretaceous Switzerland
Geology of the AlpsIchnofossiliferous formationsLimestone formations
Schrattenkalk
Schrattenkalk

The Schrattenkalk Formation is a Barremian to Aptian geologic formation in the Alps. The limestone is highly karstified. Fossil ornithopod tracks have been reported from the formation. Iguanodont tracks have been registered in the Swiss portion of the formation. The famous north face of the Eiger is partly composed of Schrattenkalk, as well as the Sturmannshöhle in southernmost Bavaria, Germany, and the Hölloch (second-longest cave in Europe) and Silberen system karst caves in Switzerland.

Excerpt from the Wikipedia article Schrattenkalk Formation (License: CC BY-SA 3.0, Authors, Images).

Schrattenkalk Formation
Lopperstrasse,

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Wikipedia: Schrattenkalk FormationContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 46.9751 ° E 8.3303 °
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Lopperstrasse
6362
Nidwalden, Switzerland
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Schrattenkalk
Schrattenkalk
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