Logo link to homepage

Report on Izu-Oshima (Japan) — November 1990

Bulletin of the Global Volcanism Network, vol. 15, no. 11 (November 1990)
Managing Editor: Lindsay McClelland.

Izu-Oshima (Japan) Steam emission continues but seismicity declines

Please cite this report as:

Global Volcanism Program, 1990. Report on Izu-Oshima (Japan). In: McClelland, L. (ed.), Bulletin of the Global Volcanism Network, 15:11. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199011-284010.

Volcano Profile |  Complete Bulletin


Izu-Oshima

Japan

34.724°N, 139.394°E; summit elev. 758 m

All times are local (unless otherwise noted)


Seismicity declined rapidly after . . . 4 October (figure 22). No additional eruptions had occurred as of early December. Steam emission continued steadily through November, with the plume reaching 1,300 m above the crater. A series of 10 microearthquakes, centered in the E part of Oshima Island 3 km E of the summit (Mihara-yama) cone occurred 7-10 November, the first seismicity there since 21 November 1987. Seismicity at the summit continued unchanged through November at relatively low levels. A seismometer near the summit recorded 160 earthquakes during November, down from 633 in October. Seismicity and steam emission remained similar in early December. No tremor has been recorded since late April.

Figure (see Caption) Figure 22. Daily number of earthquakes at Oshima, April-November 1990. The small 4 October eruption (arrow) was accompanied by high seismicity. Most of the earthquakes were centered on the summit (Mihara-yama) cone. Courtesy of JMA.

Geologic Background. Izu-Oshima volcano in Sagami Bay, east of the Izu Peninsula, is the northernmost of the Izu Islands. The broad, low stratovolcano forms an 11 x 13 km island and was constructed over the remnants of three dissected stratovolcanoes. It is capped by a 4-km-wide caldera with a central cone, Miharayama, that has been the site of numerous historical eruptions. More than 40 cones are located within the caldera and along two parallel rift zones trending NNW-SSE. Although it is a dominantly basaltic volcano, strong explosive activity has occurred at intervals of 100-150 years throughout the past few thousand years. Historical activity dates back to the 7th century CE. A major eruption in 1986 produced spectacular lava fountains up to 1600 m height and a 16-km-high eruption column; more than 12,000 people were evacuated from the island.

Information Contacts: JMA.