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...
I tiakina i:
| Ngā kaituhi matua: | , , |
|---|---|
| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Groupe français de géomorphologie
2012
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| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.4000/geomorphologie.10034 https://hdl.handle.net/20.500.13089/gipz https://journals.openedition.org/geomorphologie/10034 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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