Segnalazione di sedimenti eolici nei pressi di Bolognola (Monti Sibillini, Appennino umbro-marchigiano)

Eolian deposits in the Bolognola area (Sibillini mountains, Umbria-Marche Apennine)

Authors

  • Piero Farabollini Dipartimento di Scienze della Terra, Università di Camerino, Camerino, Italy Author
  • Gilberto Pambianchi Dipartimento di Scienze della Terra, Università di Camerino, Camerino, Italy Author
  • Eleonora Paris Dipartimento di Scienze della Terra, Università di Camerino, Camerino, Italy Author

Keywords:

Loess, Upper Pleistocene, Sibillini Mt., Umbria-Marche Apennines

Abstract

We are reporting the find of an eolian deposit similar to loess within stratified slope detritus of cryonival origin in the north-eastern sector of the Sibillini Mountains (Umbria-Marche Apennines). Laboratory analyses of the sediments together with the geomorphological characteristics of the area suggest that sedimentation took place during the Upper Pleistocene, in a cold and arid environment, the source being mostly local and, to a lesser extent, coming from adjacent volcanic areas.

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Published

2024-07-10

Issue

Vol. 13 No. 1 (1990)

Section

Short communication

License

Copyright (c) 2024 Piero Farabollini, Gilberto Pambianchi, Eleonora Paris (Author)

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