Report on Kirishimayama (Japan) — September 1995
Bulletin of the Global Volcanism Network, vol. 20, no. 9 (September 1995)
Managing Editor: Richard Wunderman.
Kirishimayama (Japan) Seismicity decreases near Shinmoe Crater
Please cite this report as:
Global Volcanism Program, 1995. Report on Kirishimayama (Japan). In: Wunderman, R (ed.), Bulletin of the Global Volcanism Network, 20:9. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199509-282090.
31.934°N, 130.862°E; summit elev. 1700 m
All times are local (unless otherwise noted)
The total number of earthquakes in September was 182, a significant decreased compared to the 463 recorded in August. On 29 September there were 25 earthquakes recorded at Station A, 1.7 km SW of Shinmoe-dake Crater, the highest daily total of the month.
Geologic Background. Kirishimayama is a large group of more than 20 Quaternary volcanoes located north of Kagoshima Bay. The late-Pleistocene to Holocene dominantly andesitic group consists of stratovolcanoes, pyroclastic cones, maars, and underlying shield volcanoes located over an area of 20 x 30 km. The larger stratovolcanoes are scattered throughout the field, with the centrally located Karakunidake being the highest. Onamiike and Miike, the two largest maars, are located SW of Karakunidake and at its far eastern end, respectively. Holocene eruptions have been concentrated along an E-W line of vents from Miike to Ohachi, and at Shinmoedake to the NE. Frequent small-to-moderate explosive eruptions have been recorded since the 8th century.
Information Contacts: Volcanological Division, Seismological and Volcanological Department, Japan Meteorological Agency (JMA), 1-3-4 Ote-machi, Chiyoda-ku, Tokyo 100 Japan.