Sub-Boreal aggradation along the Apennine margin of the Central Po Plain: geomorphological and geoarchaeological aspects

The Apennine foothills at the southern limit of the Po Plain consist of a belt of coalescent, gravelly, alluvial fans, trending to the north, towards the depocenter of the plain. Their aggradation is generally considered to have been controled by climate and linked to the glacial periods of the Midd...

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Detalles Bibliográficos

Principais autores:	Cremaschi, Mauro, Nicosia, Cristiano
Formato:	Artigo
Idioma:	Inglês
Publicado:	Groupe français de géomorphologie 2012
Assuntos:	Holocène cônes alluviaux géoarchéologie géomorphologie fluviale plaine du Pô micromorphologie des sols alluvial fans Holocene geoarchaeology alluvial geomorphology Po Plain soil micromorphology
Acceso en liña:	https://doi.org/10.4000/geomorphologie.9810 https://hdl.handle.net/20.500.13089/gipl https://journals.openedition.org/geomorphologie/9810
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