Contributo alla conoscenza della sedimentazione delle alluvioni quaternarie del Fiume Foglia (Marche)
A contribute concerning the sedimentary phenomena in Quaternary alluvial deposits of Foglia River (Northern Marche)
Keywords:
Continental sedimentation, 14C dating, MarcheAbstract
Some depositional hypothesis with radiometer datings of a fossil wood (Ulmus) (10.090 ± 80 Y.B.P.) discovered 11,5 m deep in alluvial sediments of the Foglia river, have been expressed. Through laboratory tests as with oedometer compression, the range of preconsolidation pressure, have been obtained. Results shown indicate a Holocene erosion phase which removed a part of the terrace, where the wood was deposited. A successive sedimentary cycle has accumulated new alluvial sediments.
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Published
1988-12-31
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Short communication
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Copyright (c) 1988 Umberto Gori (Author)
This work is licensed under a Creative Commons Attribution 4.0 International License.
The content is released under a CC BY-NC-ND 4.0 licence (Attribution-NonCommercial-NoDerivatives 4.0 International).
How to Cite
Gori, U. (1988). Contributo alla conoscenza della sedimentazione delle alluvioni quaternarie del Fiume Foglia (Marche): A contribute concerning the sedimentary phenomena in Quaternary alluvial deposits of Foglia River (Northern Marche). Geografia Fisica E Dinamica Quaternaria, 11(2), 121-122. https://www.gfdq.glaciologia.it/index.php/GFDQ/article/view/840
