Valley of the Nyerges Creek

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Origin: Miocene, Eggenburgian.

Geomorphological features: In Szécsényfelfalu, north of the Felső-Nyeges steppe, in the excavation of the valley of the Nyerges stream, the sediment of the Zagyvapálfalva Formation settles on the Szécsényi Slír, both of which contain microfauna.

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