JDR Vol.3 No.4 pp. 270-275
doi: 10.20965/jdr.2008.p0270


First Steps in Understanding Caldera Forming Eruptions

Tsuneomi Kagiyama* and Yuichi Morita**

*Aso Volcanological Laboratory, Graduate School of Science, Kyoto University, Minami-Aso, Aso, Kumamoto 869-1404, Japan

**Earthquake Research Insitute, University of Tokyo, Yayoi, 1-1-1 Bunkyo-ku, Tokyo 113-0032, Japan

March 31, 2008
July 6, 2008
August 1, 2008
caldera forming eruption, diversity of eruption process, failed eruption, resistivity structure of volcano
Caldera forming eruptions are characterized by a large-scale and low frequency. To prepare for them, monitoring of volcanic activity is insufficient for practical evaluation. Volcanic activity generally involves two end members, one in which an eruption dominates and one in which geothermal activity dominates, as defined by the ease in magma ascent. Caldera forming eruptions tend to be prepared where magma stagnates easily. Research on stop of magma ascent and its accumulation is required to understand caldera forming eruptions.
Cite this article as:
T. Kagiyama and Y. Morita, “First Steps in Understanding Caldera Forming Eruptions,” J. Disaster Res., Vol.3 No.4, pp. 270-275, 2008.
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