![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, Sarmatian and Upper Pleistocene.
Geomorphological features: In the Szirák Dózsa György út sand mine, the sediments were accumulated by constant watercourse with a gradually decreasing energy. As a result, a large number of mollusks accumulated from the sand, accumulated from the Sarmatian sediments, as well as Mollusca and small vertebrate remains, suggesting a period of river activity (risszwürm interglacial).