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A relict sand‐wedge polygon site in north‐central Hungary

Author

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  • János Kovács
  • Szabolcs Ákos Fábián
  • Ferenc Schweitzer
  • Gábor Varga

Abstract

Relict sand‐wedge polygons are described from palaeosol and gravel deposits in the Mogyoród area, Hungary. Based on previously reported periglacial features, the local glacial history and optically stimulated luminescence (OSL) dates, these features suggest that the Pannonian Basin was underlain by permafrost during the Late Pleniglacial (22 000–18 000 years ago) and that the permafrost may have been continuous. Copyright © 2007 John Wiley & Sons, Ltd.

Suggested Citation

  • János Kovács & Szabolcs Ákos Fábián & Ferenc Schweitzer & Gábor Varga, 2007. "A relict sand‐wedge polygon site in north‐central Hungary," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 18(4), pages 379-384, October.
    • Handle: RePEc:wly:perpro:v:18:y:2007:i:4:p:379-384
    DOI: 10.1002/ppp.600
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    Cited by:

    1. Juan Pedro Rodríguez-López & Chihua Wu & Tatiana A. Vishnivetskaya & Julian B. Murton & Wenqiang Tang & Chao Ma, 2022. "Permafrost in the Cretaceous supergreenhouse," Nature Communications, Nature, vol. 13(1), pages 1-15, December.

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