http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28604
Morpho-structural setting of Stromboli volcano revealed by high-resolution bathymetry and backscatter data of its submarine portions (Articolo in rivista)
- Type
- Label
- Morpho-structural setting of Stromboli volcano revealed by high-resolution bathymetry and backscatter data of its submarine portions (Articolo in rivista) (literal)
- Anno
- 2009-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00445-009-0279-5 (literal)
- Alternative label
Bosman A., Chiocci F.L., Romagnoli C. (2009)
Morpho-structural setting of Stromboli volcano revealed by high-resolution bathymetry and backscatter data of its submarine portions
in Bulletin of volcanology (Print)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bosman A., Chiocci F.L., Romagnoli C. (literal)
- Pagina inizio
- Pagina fine
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- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- electonic supplementary material:
Bathymorphological Map of Stromboli Volcano (Italy). Side Scan Sonar Tobi Mosaic of Stromboli Volcano. (literal)
- Note
- Scopu (literal)
- Google Scholar (literal)
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Bosman A.:CNR-IGAG, Istituto di Geologia Ambientale e Geoingegneria, Area della Ricerca di Roma 1, Dip. Scienze della Terra, University of Roma \"La Sapienza\";
Chiocci F.L.: Dip. Scienze della Terra, University of Roma \"La Sapienza\", CNR-IGAG, Istituto di Geologia Ambientale e Geoingegneria, Area della Ricerca di Roma 1;
Romagnoli C.: Dip. Scienze della Terra e Geologico-Ambientali, University of Bologna (literal)
- Titolo
- Morpho-structural setting of Stromboli volcano revealed by high-resolution bathymetry and backscatter data of its submarine portions (literal)
- Abstract
- The first high-resolution bathymetric and backscatter maps of offshore Stromboli Island are presented,
together with an interpretation of its volcanic, structural and
sedimentary features. The volcanic edifice is characterized
by a sub-conical shape with a quasi-bilateral symmetry with
respect to a NE-SW axis. The dimensions of the Strombolicchio volcanic centre, to the NE of Stromboli, have been
restored by redrawing its morphology before wave action
that eroded it in Late Quaternary time. On the NE
submarine flank of Strombolicchio, a N64°E structural
trend controls the shape of Strombolicchio Canyon. On the
southern side of Stromboli, the submarine flank has a radial
structural trend, possibly reflecting a volcanic stress regime.
Landslide scars at various scales are ubiquitous on the
submarine slopes of Stromboli. Repeated large-scale lateral
collapses have affected both the northwestern and southeastern unbuttressed flanks of the volcano, producing large
debris avalanche deposits (literal)
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