Deep-Sea Deposits of the Stromboli 30 December 2002 Landslide (Articolo in rivista)

Type

• Prodotto della ricerca (Classe)
• Articolo in rivista (Classe)

Label

• Deep-Sea Deposits of the Stromboli 30 December 2002 Landslide (Articolo in rivista) (literal)

Anno

• 2008-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.1029/182GM14 (literal)

Alternative label

• Marani, Michael P.; Gamberi, Fabiano; Rosi, Mauro; Bertagnini, Antonella; Di Roberto, Alessio (2008)
  Deep-Sea Deposits of the Stromboli 30 December 2002 Landslide
  in Geophysical monograph
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Marani, Michael P.; Gamberi, Fabiano; Rosi, Mauro; Bertagnini, Antonella; Di Roberto, Alessio (literal)

Pagina inizio

• 157 (literal)

Pagina fine

• 169 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 182 (literal)

Rivista

• Geophysical monograph (Rivista)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali

• 13 (literal)

Note

• ISI Web of Science (WOS) (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• Consiglio Nazionale delle Ricerche (CNR); Ist Nazl Geofis & Vulcanol; University of Pisa (literal)

Titolo

• Deep-Sea Deposits of the Stromboli 30 December 2002 Landslide (literal)

Abstract

• Stromboli is a 3000-m-high island-arc volcano rising to 900 m above sea level. It is the most active volcano of the Aeolian archipelago in the Tyrrhenian Sea (Italy). In the last 13 ka, four large-volume (1-km(3)) flank collapses have shaped the northwestern flank [Sciara del Fuoco (SdF)] of the volcano with the potential to cause hazardous tsunamis. In addition, smaller volume, more frequent partial collapses of the SdF have been shown to be tsunami-generating events. One such partial collapse occurred on 30 December 2002. The resulting landslide generated a 10-m-high tsunami that impacted the island. Multibeam bathymetry, side-scan sonar, and seabed visual observations reveal that 25-30 x 10(6) m(3) of sediments were deposited on the offshore from the SdF landslide. Samples have led to the recognition of a proximal coarse-grained landslide deposit on the volcano slope and a distal, cogenetic, sandy turbidite 24 km from the Stromboli shoreline. The proximal landslide deposit consists of two contiguous facies: (1) a chaotic, coarse-grained deposit and (2) a sand facies that develops laterally with and over the coarse-grained deposits. Distally, a capping 2- to 3-cm-thick sand layer, not present in a prelandslide September 2002 core, represents the finer-grained turbidite equivalent to the proximal deposits. Characteristics of the SdF landslide deposits suggest that they derive from cohesionless, sandy matrix density flows. A range of density flow transitions, based principally on particle concentration and grain-size partitioning of cohesionless parent flows, can be identified in the proximal and distal deposits of this relatively small-scale landslide event on Stromboli. (literal)

Prodotto di

• Marine science institute (ISMAR) (Istituto)

Autore CNR

• MICHAEL MARANI (Unità di personale interno)
• FABIANO GAMBERI (Persona)

Incoming links:

Autore CNR di

• FABIANO GAMBERI (Persona)
• MICHAEL MARANI (Unità di personale interno)

Prodotto

• Marine science institute (ISMAR) (Istituto)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Geophysical monograph (Rivista)