Report on Fujisan (Japan) — September 2001
Bulletin of the Global Volcanism Network, vol. 26, no. 9 (September 2001)
Managing Editor: Richard Wunderman.
Fujisan (Japan) April-May 2001 earthquakes located at 15 km depth NE of the summit
Please cite this report as:
Global Volcanism Program, 2001. Report on Fujisan (Japan). In: Wunderman, R. (ed.), Bulletin of the Global Volcanism Network, 26:9. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN200109-283030.
35.361°N, 138.728°E; summit elev. 3776 m
All times are local (unless otherwise noted)
Earthquakes increased at Fuji during April-May 2001. According to the Japan Meteorological Agency 67 earthquakes were detected on 30 April. This was the highest daily number since the 53 that occurred on 18 December 2000, even though seismic activity had been relatively low since the beginning of the year. During the week of 3-9 May 2001 the number of weekly earthquakes was as high as 130. Since September 2000 most of the earthquakes were of low magnitude and low frequency. Their hypocenters were NE of the summit at ~15 km depth. The monitoring system of National Research Institute for Earth Science and Disaster Prevention had not detected any other anomalous signs.
Geologic Background. The conical form of Fujisan, Japan's highest and most noted volcano, belies its complex origin. The modern postglacial stratovolcano is constructed above a group of overlapping volcanoes, remnants of which form irregularities on Fuji's profile. Growth of the Younger Fuji volcano began with a period of voluminous lava flows from 11,000 to 8000 years before present (BP), accounting for four-fifths of the volume of the Younger Fuji volcano. Minor explosive eruptions dominated activity from 8000 to 4500 BP, with another period of major lava flows occurring from 4500 to 3000 BP. Subsequently, intermittent major explosive eruptions occurred, with subordinate lava flows and small pyroclastic flows. Summit eruptions dominated from 3000 to 2000 BP, after which flank vents were active. The extensive basaltic lava flows from the summit and some of the more than 100 flank cones and vents blocked drainages against the Tertiary Misaka Mountains on the north side of the volcano, forming the Fuji Five Lakes, popular resort destinations. The last confirmed eruption of this dominantly basaltic volcano in 1707 was Fuji's largest during historical time. It deposited ash on Edo (Tokyo) and formed a large new crater on the east flank.
Information Contacts: National Research Institute for Earth Science and Disaster Prevention, 3-1 Tennodai, Tsukuba-shi, Ibaraki-ken, 305, Japan (URL: http://www.bosai.go.jp/); Setsuya Nakada, Hidefumi Watanabe, and Shin-ichi Sakai, Volcano Research Center, Earthquake Research Institute, University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japan (URL: http://www.eri.u-tokyo.ac.jp/VRC/index_E.html); Japan Meteorological Agency, Volcanological Division, 1-3-4 Ote-machi, Chiyoda-ku, Tokyo 100, Japan (URL: http://www.jma.go.jp/).