http://www.cnr.it/ontology/cnr/individuo/prodotto/ID135542
The landslide sequence induced by the 2002 eruption at Stromboli volcano (Contributo in volume (capitolo o saggio))
- Type
- Label
- The landslide sequence induced by the 2002 eruption at Stromboli volcano (Contributo in volume (capitolo o saggio)) (literal)
- Anno
- 2005-01-01T00:00:00+01:00 (literal)
- Alternative label
Tommasi P., Baldi P., Chiocci F.L., Coltelli M., Marsella M., Pompilio M., Romagnoli C. (2005)
The landslide sequence induced by the 2002 eruption at Stromboli volcano
Springer, Berlin (Germania) in Landslides: Risk Analysis and Sustainable Disaster Management, 2005
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Tommasi P., Baldi P., Chiocci F.L., Coltelli M., Marsella M., Pompilio M., Romagnoli C. (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
- Landslides: Risk Analysis and Sustainable Disaster Management (literal)
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- CNR-IGAG
Università di Bologna
Università Sapienza, Roma
INGV-Catania
Università Sapienza, Roma
INGV-Pisa
Università di Bologna (literal)
- Titolo
- The landslide sequence induced by the 2002 eruption at Stromboli volcano (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#inCollana
- Landslide - Risk analysis and sustainable disaster management (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#curatoriVolume
- Kyoji Sassa, Hiroshi Fukuoka, Fawu Wang, Gonghui Wang (literal)
- Abstract
- The complex sequence of large-scale tsunamogenic instability phenomena occurred on the subaerial and submarine NW flank of the Stromboli Volcano soon after the beginning of the December 2002 eruption is reconstructed and its relationship with volcanic activity is evidenced. After a brief description of slope morphology and stratigraphy, geometry and kinematics of the landslides are described. Finally, instability mechanisms that controlled the subaerial and submarine slope failures are proposed with reference to the different geotechnical, hydraulic, and loading/strain conditions that characterized the different stages of the slope evolution. (literal)
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