Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8955
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dc.contributor.authorallNeri, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallLe Cozannet, G.; Bur Rech Geol & Minieres, F-45060 Orleans, Franceen
dc.contributor.authorallThierry, P.; Bur Rech Geol & Minieres, F-45060 Orleans, Franceen
dc.contributor.authorallBignami, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallRuch, J.; Univ Roma Tre, Dipartimento Sci, Rome, Italyen
dc.date.accessioned2014-02-28T12:23:46Zen
dc.date.available2014-02-28T12:23:46Zen
dc.date.issued2013en
dc.identifier.urihttp://hdl.handle.net/2122/8955en
dc.description.abstractHazard mapping in poorly known volcanic areas is complex since much evidence of volcanic and non-volcanic hazards is often hidden by vegetation and alteration. In this paper, we propose a semi-quantitative method based on hazard event tree and multi-hazard map constructions developed in the frame of the FP7 MIAVITA project. We applied this method to the Kanlaon volcano (Philippines), which is characterized by poor geologic and historical records. We combine updated geological (long-term) and historical (short-term) data, building an event tree for the main types of hazardous events at Kanlaon and their potential frequencies. We then propose an updated multi-hazard map for Kanlaon, which may serve as a working base map in the case of future unrest. The obtained results extend the information already contained in previous volcanic hazard maps of Kanlaon, highlighting (i) an extensive, potentially active ~5 km long summit area striking north–south, (ii) new morphological features on the eastern flank of the volcano, prone to receiving volcanic products expanding from the summit, and (iii) important riverbeds that may potentially accumulate devastating mudflows. This preliminary study constitutes a basis that may help local civil defence authorities in making more informed land use planning decisions and in anticipating future risk/hazards at Kanlaon. This multi-hazard mapping method may also be applied to other poorly known active volcanoes.en
dc.description.sponsorshipThis work was undertaken under the MIAVITA project, financed by the European Commission under the 7th Framework Programme for Research and Technological Development, Area “Environment”, Activity 6.1 “Climate Change, Pollution and Risks”.en
dc.language.isoEnglishen
dc.publisher.nameCOPERNICUS GESELLSCHAFT MBH, BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANYen
dc.relation.ispartofNatural Hazards and Earth System Sciences (NHESS)en
dc.relation.ispartofseries8/13 (2013)en
dc.subjectRISK ASSESSMENTSen
dc.subjectMount Kanlaonen
dc.titleA method for multi-hazard mapping in poorly known volcanic areas: an example from Kanlaon (Philippines)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1929-1943en
dc.identifier.URLhttp://www.nat-hazards-earth-syst-sci.net/13/1929/2013/nhess-13-1929-2013.htmlen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneousen
dc.identifier.doi10.5194/nhess-13-1929-2013en
dc.description.obiettivoSpecifico1V. Storia e struttura dei sistemi vulcanicien
dc.description.obiettivoSpecifico2V. Dinamiche di unrest e scenari pre-eruttivien
dc.description.obiettivoSpecifico3V. Dinamiche e scenari eruttivien
dc.description.obiettivoSpecifico4V. Vulcani e ambienteen
dc.description.obiettivoSpecifico6A. Monitoraggio ambientale, sicurezza e territorioen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.relation.issn1561-8633en
dc.relation.eissn1684-9981en
dc.contributor.authorNeri, M.en
dc.contributor.authorLe Cozannet, G.en
dc.contributor.authorThierry, P.en
dc.contributor.authorBignami, C.en
dc.contributor.authorRuch, J.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentBur Rech Geol & Minieres, F-45060 Orleans, Franceen
dc.contributor.departmentBur Rech Geol & Minieres, F-45060 Orleans, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentUniv Roma Tre, Dipartimento Sci, Rome, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.dept1BRGM, French Geological Survey, 3 avenue Claude Guillemin, 45100 Orléans, France-
crisitem.author.deptBur Rech Geol & Minieres, F-45060 Orleans, France-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptDipartimento Scienze Geologiche, Università Roma Tre, Roma, Italy-
crisitem.author.orcid0000-0002-5890-3398-
crisitem.author.orcid0000-0002-8632-9979-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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