The outline of the 2011 eruption at Shinmoe-dake (Kirishima), Japan

Setsuya Nakada, Masashi Nagai, Takayuki Kaneko, Yuki Suzuki, Fukashi Maeno

研究成果: Article査読

56 被引用数 (Scopus)

抄録

The climactic phase of the 2011 eruption at Shinmoe-dake was a mixture of subplinian and vulcanian eruptive events, successive lava accumulation (lava dome) within the crater, and repetition of vulcanian events after the dome growth. It was preceded by inflation and elevated seismicity for about one year and by phreatomagmatic explosions of one week before. Small pyroclastic flows and ash-cloud surges formed during the subplinian events, when the eruption column reached the highest level and the vent was widened. A lava dome, which was extruded close to the vent of subplinian events, grew by swelling upward and filling the crater. After the vent was covered by the lava, an intense vulcanian event occurred from the base of the dome and the swelled dome became deflated. After that, vulcanian events were repeated for three months. Simultaneous eruption styles in the crater (vulcanian events, continuous ash emission and dome growth) and some phreatomagmatic events in the vulcanian stage probably are due to a complex upper-conduit system developed in water-saturated country rock.

本文言語English
ページ(範囲)475-488
ページ数14
ジャーナルEarth, Planets and Space
65
6
DOI
出版ステータスPublished - 2013
外部発表はい

ASJC Scopus subject areas

  • 地質学
  • 宇宙惑星科学

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