https://m2.mtmt.hu/ eng 2026-04-15 00:10 JournalArticle 1384782 APPROVED true 0 2018-09-13T04:18:19.000+0000 false 1384782 2026-03-26T11:46:49.181+0000 2025-04-17T19:43:27.858+0000 2010-10-20T08:16:46.000+0000 true 10015050 Németh Károly /api/author/10015050 Author Károly Németh (Vulkanológia, szedimentológia) true 10015050 2022-11-11T08:56:06.536+0000 Admin 10003133 /api/admin/10003133 Annamária Boros (MTMT Központi admin) Boros Annamária true 10003133 true 2022-03-22T18:24:48.781+0000 true false true 24 24 /api/publicationtype/24 PublicationType Journal Article 1 true 24 JournalArticle true 10000059 Article true 24 24 /api/publicationtype/24 PublicationType Journal Article 1 true 24 JournalArticle /api/subtype/10000059 Szakcikk SubType Article (Journal Article) 101 true 10000059 true 1 /api/category/1 Category Scientific true 1 Németh, K true true /api/journal/2944 REVIEWED JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 true false 2944 false 2944 true 0377-0273 1872-6097 Journal FOREIGN 180 2-4 246 258 246 13 2009 Ambae Island is a mafic stratovolcano located in the northern Vanuatu volcanic arc and has a NE-SW rift-controlled elongated shape. Several hundred scoria cones and fissure-fed lava fields occur along its long axis. After many decades of quiescence, Ambae Island erupted on the 28th of November 2005, disrupting the lives of its 10,000 inhabitants. Its activity remained focused at the central (crater-lake filled) vent and this is where hazard-assessments were focused. These assessments initially neglected that maars, tephra cones and rings occur at each tip of the island where the eruptive activity occurred < 500 and < 300 yr B.P. The products of this explosive phreatomagmatic activity are located where the rift axis meets the sea. At the NE edge of the island five tephra rings occur, each comparable in size to those on the summit of Ambae. Along the NE coastline, a near-continuous cliff section exposes an up to 25 m thick succession of near-vent phreatomagmatic tephra units derived from closely spaced vents. This can be subdivided into two major lithofacies associations. The first association represents when the locus of explosions was below sea level and comprises matrix-supported, massive to weakly stratified beds of coarse ash and lapilli. These are dominant in the lowermost part of the sequence and commonly contain coral fragments, indicating that the loci of explosion were located within a reef or coral sediment near the syn-eruptive shoreline. The second type indicate more stable vent conditions and rapidly repeating explosions of high intensity, producing fine-grained tephra with undulatory bedding and cross-lamination as well as megaripple bedforms. These surge and fall beds are more common in the uppermost part of the succession and form a few-m-thick pile. An older tephra succession of similar character occurs below, and buried trees in growth position, as well as those flattened within base surge beds. This implies that the centre of this eruption was very near the coastline. The processes implied by these deposits are amongst the most violent forms of volcanism on this island. In addition, the lowland and coastal areas affected by these events are the most heavily populated. This circumstance is mirrored on many similar volcanic islands, including the nearby SW Pacific examples of Taveuni (Fiji), Upolu and Savai'i (Samoa), and Ambrym (Vanuatu). These locations are paradoxically often considered safe areas during summit/central-vent eruptions, simply because they are farthest from the central sources of ash-fall and lahar hazard. The observations presented here necessitate a revision of this view. © 2008 Elsevier B.V. All rights reserved. 2010 true true true false false NONE 2026-03-26 false 29 0 27 13 3 27 26 24 19 26 26 12 12 15 14 0 29 15 27 13 0 8 8 Folyóiratcikk Journal Article 24 26 Könyvrészlet Chapter in Book 25 1 Könyv Book 23 0 Egyéb konferenciaközlemény Conference paper 31 0 Egyéb konferenciakötet Conference proceedings 32 0 Oltalmi formák Protection forms 26 0 Disszertáció Thesis 28 2 Egyéb Miscellaneous 29 0 Alkotás Achievement 22 0 Kutatási adat Research data 33 0 Folyóiratcikk Journal Article 24 0 0 0 Könyvrészlet Chapter in Book 25 0 0 0 Könyv Book 23 0 0 0 Egyéb konferenciaközlemény Conference paper 31 0 0 0 Egyéb konferenciakötet Conference proceedings 32 0 0 0 Oltalmi formák Protection forms 26 0 0 0 Disszertáció Thesis 28 0 0 0 Egyéb Miscellaneous 29 0 0 0 Alkotás Achievement 22 0 0 0 Kutatási adat Research data 33 0 0 0 2009 0 2 0 2 0 2010 0 2 1 2 1 2011 0 1 0 1 0 2012 0 1 1 1 1 2013 0 1 1 1 1 2014 0 2 1 2 1 2015 0 2 0 2 0 2016 0 2 1 2 1 2017 0 0 0 0 0 2018 0 1 0 1 0 2019 0 2 1 2 1 2020 0 4 3 4 3 2021 0 2 1 2 1 2022 0 3 2 3 2 2023 0 0 0 0 0 2024 0 2 2 2 2 2025 0 2 1 2 1 Q1 A false false false false 2013-01-03T01:24:08.000+0000 2012-10-05T00:24:08.000+0000 1 2 0 2 0 true 10003133 Language 10002 /api/language/10002 English Angol English true 2 true PersonAuthorship 1086892 /api/authorship/1086892 Németh, K [Németh, Károly (Vulkanológia, sze...), author] 1 0.5 true false Author 10015050 /api/author/10015050 Károly Németh (Vulkanológia, szedimentológia) Németh Károly true 10015050 true Németh K true false false AuthorshipType 1 /api/authorshiptype/1 Author 0 true 0 true false 11236137 true PersonAuthorship 1086893 /api/authorship/1086893 Cronin, S J 2 0.5 false true Cronin S J true false false AuthorshipType 1 /api/authorshiptype/1 Author 0 true 0 true false 11236136 true PublicationIdentifier 299280 /api/publicationidentifier/299280 DOI: 10.1016/j.jvolgeores.2008.08.011 PlainSource 6 /api/publicationsource/6 DOI PublicationSourceType 10001 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http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-61849112866 true true Classification 10399 /api/classification/10399 Earth and related Environmental sciences true true Keyword 4945 /api/keyword/4945 Seawater true 4945 true Keyword 17229 /api/keyword/17229 BASALT true 17229 true Keyword 1002813 /api/keyword/1002813 base surge true 1002813 true Keyword 1002814 /api/keyword/1002814 accretionary lapilli true 1002814 true Keyword 1002815 /api/keyword/1002815 sideromelane true 1002815 true Keyword 1002816 /api/keyword/1002816 scoria true 1002816 true Keyword 1002817 /api/keyword/1002817 rift true 1002817 true Keyword 1002818 /api/keyword/1002818 tuff cone true 1002818 true Keyword 1002831 /api/keyword/1002831 tuff ring true 1002831 true Keyword 1002843 /api/keyword/1002843 phreatomagmatic true 1002843 true Keyword 1002844 /api/keyword/1002844 volcanic island true 1002844 true Keyword 1002868 /api/keyword/1002868 Vanuatu true 1002868 true Keyword 1002891 /api/keyword/1002891 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Explosions true 1003066 true Keyword 1003067 /api/keyword/1003067 Coastal zones true 1003067 true MtaRating 11435122 /api/mtarating/11435122 X. Section of Earth Sciences:A JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 RatingType 10031 /api/ratingtype/10031 X. Section of Earth Sciences X. FTO Institute 70 /api/institute/70 HAS Section of Earth Sciences (X.) HASSESX 0 false false false X. Földtudományok Osztálya HAS Section of Earth Sciences (X.) true 70 true true true A true true SjrRating 5793903 /api/sjrrating/5793903 sjr:Q1 (2009) Scopus - Geochemistry and Petrology JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 21 0.24 journal RatingType 10002 /api/ratingtype/10002 sjr sjr true true ClassificationExternal 1906 /api/classificationexternal/1906 Scopus - Geochemistry and Petrology true 1906 true Q1 DIRECT true 5793903 true Reference 1176957 /api/reference/1176957 1. Arana, V., Felpeto, A., Astiz, M., Garcia, A., Ortiz, R., Abella, R., Zonation of the main volcanic hazards (lava flows and ash fall) in Tenerife, Canary Islands. A proposal for a surveillance network (2000) J. Volcanol. 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(2009) JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 180 2-4 246-258<div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" mtid="10015050"><a href="/gui2/?type=authors&mode=browse&sel=10015050" target="_blank">Németh K (<span class="authorship-author-name">Németh Károly</span> <span class="authorAux-mtmt"> Vulkanológia, szedimentológia</span>) </a> </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Cronin S J </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;1384782" target="_blank">Phreatomagmatic volcanic hazards where rift-systems meet the sea, a study from Ambae Island, Vanuatu</a></div> <div> <span class="journal-title">JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0377-0273">0377-0273</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1872-6097">1872-6097</a>)</span>: <span class="journal-volume">180</span> <span class="journal-issue">2-4</span> <span class="page"> pp 246-258 </span> <span class="year">(2009)</span> </div> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Language: English | </span> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.jvolgeores.2008.08.011" target="_blank" href="https://doi.org/10.1016/j.jvolgeores.2008.08.011"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000265196400013" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000265196400013"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="61849112866" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-61849112866"> Scopus </a> </span> </span> <OnlyViewableByAuthor><div class="ratings"> <div class="journal-subject">Journal subject: Scopus - Geochemistry and Petrology&nbsp;&nbsp;&nbsp;Rank:&nbsp;Q1</div> <div class="journal-subject">Journal subject: Scopus - Geophysics&nbsp;&nbsp;&nbsp;Rank:&nbsp;Q1</div> <div class="journal-subject">HAS Section of Earth Sciences (X.) HASSESX&nbsp;&nbsp;&nbsp;A</div> </div></OnlyViewableByAuthor> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="" class="citingPub-count">Citing papers: 29</span> | Independent citation: 15 | Self citation: 14 | Unknown citation: 0 | Number of citations in WoS: 24 | Number of citations in Scopus:&nbsp;19 | WoS/Scopus assigned:&nbsp;26 | Number of citations with DOI:&nbsp;26 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;1384782&sort=publishedYear,desc&sort=title"> Number of cited publications: 8 </a> </div> <div class="mtid"><span class="long-pub-mtid">Publication: 1384782</span> | <span class="status-data status-APPROVED"> Published </span> <span class="oldId">Old id: 1384782</span> | Core Citing | <span class="type-subtype">Journal Article ( Article ) </span> | <span class="pub-category">Scientific</span> | <span class="publication-sourceOfData">kézi felvitel</span> </div> <div class="lastModified">Last Modified: 2025.04.17. 21:43 Éva Pécsi (MTMT Közp 2,3, admin) </div> <div class="lockedBy">Centrally managed 2022.03.22. 19:24 Annamária Boros (MTMT Központi admin) </div> </div></div>