Reconstruction of the 2014 eruption sequence of Ontake Volcano from recorded images and interviews
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DOI[10.1186/s40623-016-0458-5]のデータに遷移します
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- 資料種別
- 記事
- タイトル
- 著者・編者
- Teruki OikawaMitsuhiro YoshimotoSetsuya Nakada
- 出版年月日等
- 2016-05-14
- 出版年（W3CDTF）
- 2016-05-14
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 68(79)
- 掲載巻
- 68(79)
- ISSN（掲載誌）
- 1880-5981
- ISSN-L（掲載誌）
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-016-0458-5
- 国立国会図書館永続的識別子
- info:ndljp/pid/9976822
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2016-05-17T18:44:59+09:00
- 保存日（W3CDTF）
- 2016-05-17
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/9963599
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- コレクション（個別）
- 国立国会図書館デジタルコレクション > デジタル化資料 > 雑誌
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 所蔵機関
- 国立国会図書館
- 請求記号
- Z19-383
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/3421918
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- 書誌ID（NDLBibID）
- 9976822
- 整理区分コード
- 632
- 要約等
- A phreatic eruption at Mount Ontake (3067 m) on September 27, 2014, led to 64 casualties, including missing people. In this paper, we clarify the eruption sequence of the 2014 eruption from recorded images (photographs and videos obtained by climbers) and interviews with mountain guides and workers in mountain huts. The onset of eruption was sudden, without any clear precursory surface phenomena (such as ground rumbling or strong smell of sulfide). Our data indicate that the eruption sequence can be divided into three phases. Phase 1: The eruption started with dry pyroclastic density currents (PDCs) caused by ash column collapse. The PDCs flowed down 2.5 km SW and 2 km NW from the craters. In addition, PDCs moved horizontally by approximately 1.5 km toward N and E beyond summit ridges. The temperature of PDCs at the summit area partially exceeded 100 °C, and an analysis of interview results suggested that the temperature of PDCs was mostly in the range of 30–100 °C. At the summit area, there were violent falling ballistic rocks. Phase 2: When the outflow of PDCs stopped, the altitude of the eruption column increased; tephra with muddy rain started to fall; and ambient air temperature decreased. Falling ballistic rocks were almost absent during this phase. Phase 3: Finally, muddy hot water flowed out from the craters. These models reconstructed from observations are consistent with the phreatic eruption models and typical eruption sequences recorded at similar volcanoes.ArticleEarth, Planets and Space. 68:79 (2016)
- DOI
- 10.1186/s40623-016-0458-5
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- © 2016 Oikawa et al. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
- 関連情報（URI）
- 参照
- Transport of ballistic projectiles during the 2015 Aso Strombolian eruptionsMachine-learning-based detection of volcano seismicity using the spatial pattern of amplitudesLahar characteristics as a function of triggering mechanism at a seasonally snow-clad volcano: contrasting lahars following the 2014 phreatic eruption of Ontake Volcano, JapanReconstruction of a phreatic eruption on 27 September 2014 at Ontake volcano, central Japan, based on proximal pyroclastic density current and fallout depositsHydrothermal Aluminum-Phosphate-Sulfates in Ash from the 2014 Hydrothermal Eruption at Ontake Volcano, Central Honshu, JapanBuildings vs. ballistics: Quantifying the vulnerability of buildings to volcanic ballistic impacts using field studies and pneumatic cannon experimentsThe Communication and Risk Management of Volcanic Ballistic HazardsShallow Magmatic Hydrothermal Eruption in April 2018 on Ebinokogen Ioyama Volcano in Kirishima Volcano Group, Kyushu, JapanSeismic structure and its implication on the hydrothermal system beneath Mt. Ontake, central JapanResuspension of ash after the 2014 phreatic eruption at Ontake volcano, JapanA numerical model for precursory time sequences of the phreatic eruptions of Mt. Ontake, central Japan御嶽山2014年水蒸気噴火とその後の侵食水蒸気噴火の地質学的研究Conveying Volcano Information Effectively to Stakeholders – A New Project for Promotion of Next Generation Volcano ResearchSignificance of Electromagnetic Surveys at Active Volcanoes: Toward Evaluating the Imminence of Wet Eruptionsアンケート調査に基づく御嶽山2014年9月27日噴火の降灰域火山岩塊による火口近傍建物被害と即時被害調査用シートの開発模擬火山れきに対する登山用ヘルメットの耐衝撃特性水蒸気噴火発生場としての草津白根火山Consideration for Solving Problems Related to Volcanic Disaster Prevention by Real-Time Grasping of Climber MovementSuspended sediment transport diversity in river catchments following the 2014 phreatic eruption at Ontake Volcano, JapanBehavior of magmatic components in fumarolic gases related to the 2018 phreatic eruption at Ebinokogen Ioyama volcano, Kirishima Volcanic Group, Kyushu, JapanEstimation of ballistic block landing energy during 2014 Mount Ontake eruption
- 参照
- Sequence of the 1895 eruption of the Zao volcano, Tohoku JapanPyroclastic block flow from the September, 1976, eruption of La Soufrière volcano, GuadeloupeUsing the spatial distribution and lithology of ballistic blocks to interpret eruption sequence and dynamics: August 6 2012 Upper Te Maari eruption, New ZealandThe application of a calibrated 3D ballistic trajectory model to ballistic hazard assessments at Upper Te Maari, TongariroHydrothermal Processes above the Yellowstone Magma Chamber: Large Hydrothermal Systems and Large Hydrothermal ExplosionsExplosive properties of water in volcanic and hydrothermal systemsPyroclastic density current from the 1888 phreatic eruption of Bandai volcano, NE JapanHydrothermal eruptions in the Waiotapu geothermal system, New Zealand; their origin, associated breccias, and relation to precious metal mineralizationKAr age determination of late Quaternary volcanic rocks using the “mass fractionation correction procedure”: application to the Younger Ontake Volcano, central JapanCharacterization of low-temperature pyroclastic surges that occurred in the northeastern Japan arc during the late 19th centurySource mechanism of a very-long-period event at Mt Ontake, central Japan: Response of a hydrothermal system to magma intrusion beneath the summitThe boiling liquid expanding vapour explosion (BLEVE): Mechanism, consequence assessment, managementCharacteristics of hydrothermal eruptions, with examples from New Zealand and elsewhereDynamics of surges generated by hydrothermal blasts during the 6 August 2012 Te Maari eruption, Mt. Tongariro, New ZealandExperimental constraints on phreatic eruption processes at Whakaari (White Island volcano)Vegetation dieback as a proxy for temperature within a wet pyroclastic density current: A novel experiment and observations from the 6th of August 2012 Tongariro eruption毛髪の熱ダメージとその指標について御岳火山の歴史噴火記録の再検討と噴気活動の歴史記録樹木の発火限界温度について御嶽火山2014 年9 月27 日噴火で発生した火砕流
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 9976822
- NII論文ID
- 120007100314