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  1. 防災科研関係論文

Reconstruction of the 2014 eruption sequence of Ontake Volcano from recorded images and interviews

https://nied-repo.bosai.go.jp/records/3097
https://nied-repo.bosai.go.jp/records/3097
8ea365e0-9472-4978-aae3-4d63d0b152e5
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Reconstruction of the 2014 eruption sequence of Ontake Volcano from recorded images and interviews
言語
言語 eng
著者 Teruki Oikawa

× Teruki Oikawa

en Teruki Oikawa

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Mitsuhiro Yoshimoto

× Mitsuhiro Yoshimoto

en Mitsuhiro Yoshimoto

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Setsuya Nakada

× Setsuya Nakada

en Setsuya Nakada

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Fukashi Maeno

× Fukashi Maeno

en Fukashi Maeno

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Jiro Komori

× Jiro Komori

en Jiro Komori

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Taketo Shimano

× Taketo Shimano

en Taketo Shimano

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Yoshihiro Takeshita

× Yoshihiro Takeshita

en Yoshihiro Takeshita

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Yoshihiro Ishizuka

× Yoshihiro Ishizuka

en Yoshihiro Ishizuka

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Yasuhiro Ishimine

× Yasuhiro Ishimine

en Yasuhiro Ishimine

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抄録
内容記述タイプ Other
内容記述 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 degrees C, and an analysis of interview results suggested that the temperature of PDCs was mostly in the range of 30-100 degrees 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.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 68, 号 1, p. 79, 発行日 2016-05
出版者
言語 en
出版者 SPRINGER HEIDELBERG
ISSN
収録物識別子タイプ EISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-016-0458-5
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