Report on Asosan (Japan) — October 1990
Bulletin of the Global Volcanism Network, vol. 15, no. 10 (October 1990)
Managing Editor: Lindsay McClelland.
Asosan (Japan) Weak ash emission and glow; increased tremor
Please cite this report as:
Global Volcanism Program, 1990. Report on Asosan (Japan). In: McClelland, L. (ed.), Bulletin of the Global Volcanism Network, 15:10. Smithsonian Institution.
32.884°N, 131.104°E; summit elev. 1592 m
All times are local (unless otherwise noted)
No ash was erupted during October . . . . Crater 1 . . . continued to emit white steam that rose to 900 m above the crater. Weak ash emission was observed on 13 November, and glow from vents on the crater bottom was seen during fieldwork that night. The amplitude and number of volcanic tremor episodes increased in late October, reaching levels similar to September's and continuing at those levels through early November.
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: JMA.