Layers with different hardness were eroded and formed hogbacks.
There are ridges like the Hainleite and the Dün which are formed by the layers of the Unterer Muschelkalk ( Anisian ) and the Windleite which is formed by layers of the Buntsandstein ( Olenekian ).
The ridges in the middle of the plain are formed ba salt tectonics.
www.showcaves.comDurch die Abtragung haben sich Schichtkämme gebildet.
So sind z.B. die Hainleite und der Dün der Schichtkamm des Unteren Muschelkalks und die Windleite der des Buntsandsteins.
Die Erhöhungen innerhalb des Beckens sind salztektonischen Ursprungs.
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