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Report on Asosan (Japan) — September 1995

Bulletin of the Global Volcanism Network, vol. 20, no. 9 (September 1995)
Managing Editor: Richard Wunderman.

Asosan (Japan) Continued mud and water ejections and many isolated tremors

Please cite this report as:

Global Volcanism Program, 1995. Report on Asosan (Japan). In: Wunderman, R. (ed.), Bulletin of the Global Volcanism Network, 20:9. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199509-282110.

Volcano Profile |  Complete Bulletin


Asosan

Japan

32.884°N, 131.104°E; summit elev. 1592 m

All times are local (unless otherwise noted)


Throughout September the hot water pool on the floor of Naka-dake Crater 1 frequently ejected mud and water; the highest ejection rose 10 m. Many isolated tremors were recorded at Station A, 800 m W of the crater. The monthly total of isolated tremors was 6,618; only two earthquakes were detected. Continuous tremor with 0.2-0.8 µm amplitude was registered throughout the month.

Mud ejections have been reported since May 1994 (BGVN 19:05). The 24-km-wide Aso Caldera contains 15 central cones. One of these cones, Naka-dake, has erupted more than 165 times since 553 AD, the first documented historical eruption in Japan. Aso is located 75 km E of Unzen and 150 km N of Sakura-jima volcanoes.

Geologic Background. The 24-km-wide Asosan caldera was formed during four major explosive eruptions from 300,000 to 90,000 years ago. These produced voluminous pyroclastic flows that covered much of Kyushu. The last of these, the Aso-4 eruption, produced more than 600 km3 of airfall tephra and pyroclastic-flow deposits. A group of 17 central cones was constructed in the middle of the caldera, one of which, Nakadake, is one of Japan's most active volcanoes. It was the location of Japan's first documented historical eruption in 553 CE. The Nakadake complex has remained active throughout the Holocene. Several other cones have been active during the Holocene, including the Kometsuka scoria cone as recently as about 210 CE. Historical eruptions have largely consisted of basaltic to basaltic-andesite ash emission with periodic strombolian and phreatomagmatic activity. The summit crater of Nakadake is accessible by toll road and cable car, and is one of Kyushu's most popular tourist destinations.

Information Contacts: Volcanological Division, Seismological and Volcanological Department, Japan Meteorological Agency (JMA), 1-3-4 Ote-machi, Chiyoda-ku, Tokyo 100 Japan.