Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2377
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dc.contributor.authorallFavalli, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallChirico, G. D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallPapale, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallPareschi, M. T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallColtelli, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallLucaya, N.; Goma Volcano Observatory, Department of Geophysics, Lwiro, Centre de Recherche en Sciences Naturelles, Democratic Republic of Congoen
dc.contributor.authorallBoschi, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italiaen
dc.date.accessioned2007-08-27T08:23:22Zen
dc.date.available2007-08-27T08:23:22Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2377en
dc.description.abstractThe 17 January 2002 fissure eruption of Mount Nyiragongo, Democratic Republic of Congo, produced lava flows which entered and devastated the densely inhabited town of Goma. The 2002 and previous 1977 eruptions demonstrate the high level of volcanic risk in the area. We present an analysis of the susceptibility to lava flow invasion in Goma, by means of computer simulations based on the steepest descent path and probabilisticcomputed flow spreading and obstacle overcoming. The DEM is obtained from a topographic map of Goma by using the DEST algorithm. The numerical results show the distribution of probable lava flow paths from possible vents in the investigated topographic domain. Numerical simulations are validated through comparison with the mapped paths of the 2002 lava flows in Goma. The subsequent investigation includes the analysis of (1) hypothetical lava flow paths from ephemeral vents on the edge of the 2002 lava flows, (2) paths from venting along the hypothetical extension of the 2002 fissures, (3) paths in case of lava flow arrival in town from the north, and (4) changes induced by the presence of the solidified 2002 lava field. The results show the susceptibility of the different parts of the town of Goma to be invaded by future lava flows, and reveal the existence of a large area in town with minimum susceptibility and which can be invaded only in case of venting within it. The areas destroyed by the 2002 lava flows are predicted to be characterized by maximum susceptibility to lava flow invasion.en
dc.language.isoEnglishen
dc.publisher.nameAguen
dc.relation.ispartofJ. Geophys. Res.en
dc.relation.ispartofseries/111 (2006)en
dc.subjectComputer simulationsen
dc.subjectNyiragongo volcanoen
dc.titleComputer simulations of lava flow paths in the town of Goma, Nyiragongo volcano, Democratic Republic of Congoen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberB06202en
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.01. Data processingen
dc.identifier.doi10.1029/2004JB003527en
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L. Ruananza, A. B. Kampunzu, and J. Durieux (1994), Volcanological and petrological evolution of Nyiragongo volcano, Virunga volcanic field, Zaire, Bull. Volcanol., 56, 47– 61. Durieux, J. (2004a), Nyiragongo: The January 10th 1977 eruption, Acta Vulcanol., 14, 141– 143. Durieux, J. (2004b), Volcano Nyiragongo (D. R. Congo): Evolution of the crater and lava lakes from the discovery to the present, Acta Vulcanol., 14, 133– 140. Favalli, M., and M. T. Pareschi (2004), Digital elevation model construction from structured topographic data: The DEST algorithm, J. Geophys. Res., 109, F04004, doi:10.1029/2004JF000150. Favalli, M., M. T. Pareschi, A. Neri, and I. Isola (2005), Forecasting lava flow paths by a stochastic approach, Geophys. Res. Lett., 32, L03305, doi:10.1029/2004GL021718. Goma Volcano Observatory, (2002), Nyiragongo, Bull. Global Volcan. Network, 10– 27. Kasereka,M., J.-P. Bajope,M.Yalire, J.Durieux, D. Tedesco, and J. Lockwood (2002), Nyiragongo, Bull. Global Volcan. Network, 27, 9–10. Kavotha, K. S., T. Mavonga, J. Durieux, and K. Mukambilwa (2004), Towards a more detailed seismic picture of the January 17th, 2002 Nyiragongo eruption, Acta Vulcanol., 14, 15– 28. Komorowski, J. C., et al. (2004), The January 2002 flank eruption of Nyiragongo volcano (Democratic Republic of Congo): Chronology, evidence for a tectonic rift trigger, and impact of lava flows on the city of Goma, Acta Vulcanol., 14, 29– 64. Landi, P., M. Polacci, and M. Pompilio (2004), Final stages of cooling and crystallization in magmas feeding the January 2002 Nyiragongo eruption, paper presented at the EGU 1st General Assembly, Nice, France, 25– 30 April. Lockwood, J. P., and T. J. Casadevall (1994), Status of active volcanoes in the Goma area, Eastern Zaire, and associated hazards to residents and refugees, U.S. Geol. Surv. Open File Rep., 94-581, 18 pp. Miyamoto, H., and S. Sasaki (1997), Simulating lava flows by an improved cellular automata method, Comput. 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Natl. de Volcanol., Belgique, Missions Ge´ol. et Ge´ophys. aux Virunga, Minist.e de l’Educ. et de la Culture, Brussels. Von Go¨tzen, A. (1896), Durch Afrika von Ost nach West, Dietrich Reimer, Berlin. Wadge, G., P. A. V. Young, and I. J. McKendrick (1994), Mapping lava flow hazards using computer simulation, J. Geophys. Res., 99, 489– 504.en
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorFavalli, M.en
dc.contributor.authorChirico, G. D.en
dc.contributor.authorPapale, P.en
dc.contributor.authorPareschi, M. T.en
dc.contributor.authorColtelli, M.en
dc.contributor.authorLucaya, N.en
dc.contributor.authorBoschi, E.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentGoma Volcano Observatory, Department of Geophysics, Lwiro, Centre de Recherche en Sciences Naturelles, Democratic Republic of Congoen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptGoma Volcano Observatory, Department of Geophysics, Lwiro, Centre de Recherche en Sciences Naturelles, Democratic Republic of Congo-
crisitem.author.orcid0000-0002-7338-6069-
crisitem.author.orcid0000-0002-5207-2124-
crisitem.author.orcid0000-0001-7868-3946-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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