![Szikra Mezős éjszaka az Ősmaradványoknál](/media/thumbs/sz/ik/ra/szikra-mezos-ejszaka-az-osmaradvanyoknal-7c60ab84-2821857.jpg)
Szikra Mezős éjszaka az Ősmaradványoknál
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Origin: Miocene, Carpathian. Geomorphological featuresThe type section of the Egyházasgerge Formation is the exploration of a sand mine south of the settlement, with rich macrofauna. The rock layer forming the cover of the Salgótarján coalfields was formed in the offshore-coastal facies. In some cases, it starts with a basic conglomerate and gravel, then cross-layered chlamysic sands and sandstones are common. Remains of shark teeth are common in the Nagy Valley, from the quarry below Mocsáry-pen, and in the valley between Nagy-Hallgató and Körbérces. |