The interplay between adjacent Adige and Po alluvial systems and deltas in the late Holocene (Northern Italy)

The alluvial plain behind the southern Venice Lagoon, in northern Italy, is characterised by the presence of a complex network of alluvial ridges formed by the aggradation of channel deposits and natural levees. They are the geomorphological products of the interaction between the Adige and Po durin...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής

Κύριοι συγγραφείς:	Piovan, Silvia, Mozzi, Paolo, Zecchin, Massimo
Μορφή:	Artigo
Γλώσσα:	Inglês
Έκδοση:	Groupe français de géomorphologie 2012
Θέματα:	Holocène delta plaine alluviale lagune de Venise Adige Pô défluviation bourrelet alluvial Holocene alluvial plain Adige River Po River Venice Lagoon avulsion alluvial ridge
Διαθέσιμο Online:	https://doi.org/10.4000/geomorphologie.10034 https://hdl.handle.net/20.500.13089/gipz https://journals.openedition.org/geomorphologie/10034
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