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Report on Izu-Tobu (Japan) — July 1996

Bulletin of the Global Volcanism Network, vol. 21, no. 7 (July 1996)
Managing Editor: Richard Wunderman.

Izu-Tobu (Japan) Seismic activity increases

Please cite this report as:

Global Volcanism Program, 1996. Report on Izu-Tobu (Japan). In: Wunderman, R. (ed.), Bulletin of the Global Volcanism Network, 21:7. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199607-283010.

Volcano Profile |  Complete Bulletin


Izu-Tobu

Japan

34.9°N, 139.098°E; summit elev. 1406 m

All times are local (unless otherwise noted)


Seismicity at the Izu-Tobu volcano group increased in July. There were 318 earthquakes recorded in July; and the largest one was M 2.4 detected on 12 July. The Kamata seismic station in Ito City recorded 61 events on 15 July, and 45 events on 20 July. Seismicity declined after 24 July.

Geologic Background. The Izu-Tobu volcano group (Higashi-Izu volcano group) is scattered over a broad, plateau-like area of more than 400 km2 on the E side of the Izu Peninsula. Construction of several stratovolcanoes continued throughout much of the Pleistocene and overlapped with growth of smaller monogenetic volcanoes beginning about 300,000 years ago. About 70 subaerial monogenetic volcanoes formed during the last 140,000 years, and chemically similar submarine cones are located offshore. These volcanoes are located on a basement of late-Tertiary volcanic rocks and related sediments and on the flanks of three Quaternary stratovolcanoes: Amagi, Tenshi, and Usami. Some eruptive vents are controlled by fissure systems trending NW-SE or NE-SW. Thirteen eruptive episodes have been documented during the past 32,000 years. Kawagodaira maar produced pyroclastic flows during the largest Holocene eruption about 3000 years ago. The latest eruption occurred in 1989, when a small submarine crater was formed NE of Ito City.

Information Contacts: Volcanological Division, Japan Meteorological Agency, 1-3-4 Ote-machi, Chiyoda-ku, Tokyo 100, Japan