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Report on Asamayama (Japan) — May 1990

Bulletin of the Global Volcanism Network, vol. 15, no. 5 (May 1990)
Managing Editor: Lindsay McClelland.

Asamayama (Japan) Vapor emission; increased seismicity under crater

Please cite this report as:

Global Volcanism Program, 1990. Report on Asamayama (Japan). In: McClelland, L. (ed.), Bulletin of the Global Volcanism Network, 15:5. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199005-283110.

Volcano Profile |  Complete Bulletin


Asamayama

Japan

36.406°N, 138.523°E; summit elev. 2568 m

All times are local (unless otherwise noted)


There was a sudden increase in the number of recorded earthquakes on 8 March, which persisted through early June (figure 9). Most of the earthquakes were centered just beneath the active summit crater. The number of volcanic tremor episodes increased after 9 March, following 9 months without any recorded tremor. Steam emission has also increased conspicuously since early March (figure 10) and monthly mean plume heights were the largest since the last eruption in 1982-83.

Figure (see Caption) Figure 9. Daily number of recorded earthquakes at Asama, 1970-June 1990 (top), with detail showing daily recorded earthquakes during January 1989-June 1990 (bottom). Arrows mark eruptions. Courtesy of JMA.
Figure (see Caption) Figure 10. Height of steam emission from Asama, January-June 1990. Each bar represents one observation from Karuizawa Weather Station (JMA), 7.7 km SSE of the summit crater. Courtesy of JMA.

Geologic Background. Asamayama, Honshu's most active volcano, overlooks the resort town of Karuizawa, 140 km NW of Tokyo. The volcano is located at the junction of the Izu-Marianas and NE Japan volcanic arcs. The modern Maekake cone forms the summit and is situated east of the horseshoe-shaped remnant of an older andesitic volcano, Kurofuyama, which was destroyed by a late-Pleistocene landslide about 20,000 years before present (BP). Growth of a dacitic shield volcano was accompanied by pumiceous pyroclastic flows, the largest of which occurred about 14,000-11,000 BP, and by growth of the Ko-Asama-yama lava dome on the east flank. Maekake, capped by the Kamayama pyroclastic cone that forms the present summit, is probably only a few thousand years old and has an historical record dating back at least to the 11th century CE. Maekake has had several major plinian eruptions, the last two of which occurred in 1108 (Asamayama's largest Holocene eruption) and 1783 CE.

Information Contacts: JMA.