Suitcase fold

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As suitcase wrinkles in the are tectonics concentric folds referred consisting former horizontal rock layers by lateral pressure during a geological were formed long period to trapezoidal or even rectangular profiles. They have flat, horizontal vertices and steep, almost right-angled legs.

Pronounced case folds can be found, for example, at Bergmatten near Metzerlen-Mariastein in the Swiss Folded Jura , also known as the Blue Anticline , or in the Ionian Folded Country in Greece.

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