Oszkoruzsa Ditch

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Origin: Middle Miocene.

Geomorphological features: In the sections extending north of the Castle Hill of Sámsonháza that contains the type section of the Sámsonháza Formation, on both sides of the Oszkoruzsa Valley, from the gray layer rich in freshwater mollusks, Middle-Badenian vertebrate remains were found from four sites. Together with similar sites in Mátraszőlős and Utzeny, it is a key Middle Eastern Miocene vertebrate faunistic site in Hungary.

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