Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/1061
DC Field | Value | Language |
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dc.contributor.authorall | Favali, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | De Santis, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | D'Anna, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | Di Sabatino, B.; Università degli Studi “G. D’Annunzio”, Chieti Scalo, Italia | en |
dc.contributor.authorall | Sedita, M.; Istituto Nazionale di Fisica Nucleare, Laboratori Nazionali del Sud, Catania, Italia | en |
dc.contributor.authorall | Rubino, E.; Elettra TLC S.p.A., Telecom Italia Group, Roma, Italia | en |
dc.date.accessioned | 2006-03-22T17:34:51Z | en |
dc.date.available | 2006-03-22T17:34:51Z | en |
dc.date.issued | 2006-03-20 | en |
dc.identifier.uri | http://hdl.handle.net/2122/1061 | en |
dc.description.abstract | A strong earthquake occurred in 2002 offshore from the northern coast of Sicily in the Southern Tyrrhenian Sea (Italy), and was followed by a series of hundreds of aftershocks. Communications through the fibre-optic cable between Palermo and Rome were interrupted a few hours after the occurrence of the main shock. After the required technical checks, the failure point was found a few kilometres away from the seismic sequence area. A few days later, a specialised cable ship reached the failure area. One side of the cable was completely burnt, while about three kilometres of cable was found locked. Tests on slices of cable showed that the temperature at which the cable was heated went well above 700oC. We can speculate that the earthquakes triggered off the emission of a submarine lava flow that buried, trapped and burnt the fibre-optic cable. The revising of the bathymetric survey made before the cable’s deployment allowed for the identification of a seamount in the vicinity of the rupture. This structure could represent the lava flow’s source volcano. | en |
dc.format.extent | 1755277 bytes | en |
dc.format.mimetype | application/pdf | en |
dc.language.iso | English | en |
dc.relation.ispartof | Annals of geophysic | en |
dc.relation.ispartofseries | 2-3/49(2006) | en |
dc.subject | seismicity and volcanic activity in deep marine areas | en |
dc.subject | fibre-optic cable failure | en |
dc.subject | Southern Tyrrhenian Sea | en |
dc.title | A new active volcano in the Tyrrhenian Sea? | en |
dc.type | article | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology | en |
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Boschi (2004): An Atlas of Mediterranean seismicity, Ann. Geophys. (Suppl.), 47, 247-334. Weast, R.C. (Ed.) (1976-77): Handbook of Chemistry and Physics (Section B), CRC Press, Cleveland (57th edition), pp.439. | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | open | en |
dc.contributor.author | Favali, P. | en |
dc.contributor.author | De Santis, A. | en |
dc.contributor.author | D'Anna, G. | en |
dc.contributor.author | Di Sabatino, B. | en |
dc.contributor.author | Sedita, M. | en |
dc.contributor.author | Rubino, E. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.department | Università degli Studi “G. D’Annunzio”, Chieti Scalo, Italia | en |
dc.contributor.department | Istituto Nazionale di Fisica Nucleare, Laboratori Nazionali del Sud, Catania, Italia | en |
dc.contributor.department | Elettra TLC S.p.A., Telecom Italia Group, Roma, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Università degli Studi “G. D’Annunzio”, Chieti Scalo, Italia | - |
crisitem.author.dept | Istituto Nazionale di Fisica Nucleare, Laboratori Nazionali del Sud, Catania, Italia | - |
crisitem.author.dept | Elettra TLC S.p.A., Telecom Italia Group, Roma, Italia | - |
crisitem.author.orcid | 0000-0002-0810-0263 | - |
crisitem.author.orcid | 0000-0002-3941-656X | - |
crisitem.author.orcid | 0000-0002-4642-3901 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Annals of Geophysics |
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