Bulletin of Volcanology

, 75:779 | Cite as

Mechanism of small vulcanian eruptions at Suwanosejima volcano, Japan, as inferred from precursor inflations and tremor signals

  • Takeshi Nishimura
  • Masato Iguchi
  • Hiroshi Yakiwara
  • Jun Oikawa
  • Ryohei Kawaguchi
  • Hiroshi Aoyama
  • Haruhisa Nakamichi
  • Yusaku Ohta
  • Takeshi Tameguri
Research Article


We examine precursory signals of vulcanian eruptions at Suwanosejima volcano, southwest of Japan, by deploying seismic and tilt stations close to the active crater to understand the shallow conduit processes just before explosions. Vulcanian eruptions at Suwanosejima for the period from October 2009 to 2011 are often preceded by a sudden cessation of continuous tremor associated with continuous ash emissions. The amplitude of continuous tremor decreases within about 10 s, and tilt signal starts to show uplift of the active crater. Then, the pause of continuous tremor and uplift continue for about 1–2 min, and tilt amplitudes reach a few tens of nanoradians at a distance of 400 m from the active crater. As the pause time of continuous tremor before explosion becomes longer, the maximum amplitude of explosion earthquake and uplift signal become larger. Vulcanian eruptions are also observed during periods without continuous tremor. In these cases, tilt signals capture uplifts of the active crater for about 10 min before explosions and reach a few tens of nanoradians. Cessations of volcanic gas emissions are observed before some explosions during periods without continuous tremor (Mori et al. 2011). These observations suggest that pressurization in the shallow conduit is caused by an accumulation of volcanic gases and ash through the formation of ‘cap’ in the conduit, possibly composed of stiffened magma due to degassing, cooling, rheological changes, or other mechanisms.


Vulcanian eruption Tilt Tremor Volcanic gas Magma ascent Explosion Suwanosejima 



We appreciate Toshima village office for the approval of our observation at Suwanosejima volcano. Real-time monitoring by staffs of Sakurajima Volcano Research Center, Kyoto University, helped us to have safe observations at the active volcano. We thank the staffs of Kyushu Electric Engineering Consults that dug boreholes for our tilt measurement on the steep flanks of the Suwanosejima volcano. Constructive and suggestive comments by associate editor, Michael Manga, Greg Waite, and John Lyons were very helpful to improve the manuscript. Taketo Shimano provided us useful information on the property of volcanic ejecta at Suwanosejima. This study is supported by the Ministry of Education, Culture, Sports, Science, and Technology (MEXT) of Japan, under its Observation and Research Program for Prediction of Earthquakes and Volcanic Eruptions.


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Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  • Takeshi Nishimura
    • 1
  • Masato Iguchi
    • 2
  • Hiroshi Yakiwara
    • 3
  • Jun Oikawa
    • 4
  • Ryohei Kawaguchi
    • 1
  • Hiroshi Aoyama
    • 5
  • Haruhisa Nakamichi
    • 6
  • Yusaku Ohta
    • 7
  • Takeshi Tameguri
    • 2
  1. 1.Department of Geophysics, Graduate School of ScienceTohoku UniversitySendaiJapan
  2. 2.Sakurajima Volcano Research Center, Disaster Prevention Research InstituteKyoto UniversityKagoshimaJapan
  3. 3.Nansei-Toko Observatory for Earthquakes and Volcanoes, Faculty of ScienceKagoshima UniversityKagoshimaJapan
  4. 4.Earthquake Research InstituteUniversity of TokyoTokyoJapan
  5. 5.Institute of Seismology and Volcanology, Graduate School of ScienceHokkaido UniversitySapporoJapan
  6. 6.Earthquake and Volcano Research Center, Graduate School of Environmental StudiesNagoya UniversityNagoyaJapan
  7. 7.Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of ScienceTohoku UniversitySendaiJapan

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