http://www.cnr.it/ontology/cnr/individuo/prodotto/ID6787
Gravity instabilities in the Dohrn canyon (Naples Bay, Southern Tyrrhenian sea). Potential wave and run-up (tsunami) reconstruction from a fossil submarine landslide (Articolo in rivista)
- Type
- Label
- Gravity instabilities in the Dohrn canyon (Naples Bay, Southern Tyrrhenian sea). Potential wave and run-up (tsunami) reconstruction from a fossil submarine landslide (Articolo in rivista) (literal)
- Anno
- 2011-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.2478/v10096-011-0005-z (literal)
- Alternative label
Vincenzo Di Fiore; Gemma Aiello; Bruno D'Argenio (2011)
Gravity instabilities in the Dohrn canyon (Naples Bay, Southern Tyrrhenian sea). Potential wave and run-up (tsunami) reconstruction from a fossil submarine landslide
in Geologica Carpathica (Bratisl., Tlacené vyd.)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Vincenzo Di Fiore; Gemma Aiello; Bruno D'Argenio (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- lavoro in volume speciale di Geologica Carpathica dedicato al 13 Congresso RCMNS - Napoli
doi:10.2478/v10096-011
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#descrizioneSinteticaDelProdotto
- lavoro su rivista internazionale ISI con referee (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- CNR IAMC Sede di Napoli (literal)
- Titolo
- Gravity instabilities in the Dohrn canyon (Naples Bay, Southern Tyrrhenian sea). Potential wave and run-up (tsunami) reconstruction from a fossil submarine landslide (literal)
- Abstract
- We discuss a mathematical model of wave and run-up generated ancient submarine landslides in the canyons of the Bay of Naples (Magnaghi-Dohrn canyon system). The morpho-bathymetry and submarine gravity instabilities of such incisions have been investigated through the interpretation of a high resolution DEM. THe canyons are located in a sector of the bay where there is a variable interaction of volcanic activity (Phlegrean Fields and Ischia and Procida islands) with sedimentary processes due to the Sarno-Sebeto rivers. At present the Naples canyon-system is inactive, as evidenced by the Holocene sedimentary drapes deposited during the present sea-level highstand, but gravity instabilities occurred in the recent past at the canyons'heads. In particular the Dohrn Canyon is characterized by a double regressive head, while the Magnaghi Canyon shows a trilobate head, formed by the junction of three main tributary channels and coincident with the retreat of the shelf break around the 140 m isobath. The results of a simulation of failures in the above source areas shows that the amplitude of wave run-up, expressed in terms of the sea floor depth percentage, may range up to 2.5% of the water depth at the sea bottom.
The results of a simulation of failures at the above source areas show that the amplitude of wave run up, expressed in terms of the seafloor depth percentage, may range up to 2,5% of the water depth at the sea bottom. (literal)
- Prodotto di
- Autore CNR
- Insieme di parole chiave
Incoming links:
- Prodotto
- Autore CNR di
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi
- Insieme di parole chiave di