Report on Asosan (Japan) — February 1996
Bulletin of the Global Volcanism Network, vol. 21, no. 2 (February 1996)
Managing Editor: Richard Wunderman.
Asosan (Japan) Continuous tremor; crater floor still covered with water
Please cite this report as:
Global Volcanism Program, 1996. Report on Asosan (Japan) (Wunderman, R., ed.). Bulletin of the Global Volcanism Network, 21:2. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199602-282110
32.884°N, 131.104°E; summit elev. 1592 m
All times are local (unless otherwise noted)
The floor of Naka-dake Crater 1 remained covered with water in January. Seismic station A, 800 m W of the crater, recorded continuous tremor of 0.1-0.3 µm amplitude. In addition, there were 4,966 isolated tremors during the month.
Aso, a 24-km-wide caldera, produced pyroclastic-flow deposits during the Pleistocene that cover much of Kyushu. Its frequently active Naka-dake is one of a group of 15 intra-caldera cones.
Geological Summary. 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: Japan Meteorological Agency (JMA), Volcanological Division, Seismological and Volcanological Department, 1-3-4 Ote-machi, Chiyoda-ku, Tokyo 100, Japan.