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Report on Aira (Japan) — 21 August-27 August 2013

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 21 August-27 August 2013
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2013. Report on Aira (Japan). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 21 August-27 August 2013. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (21 August-27 August 2013)


Aira

Japan

31.593°N, 130.657°E; summit elev. 1117 m

All times are local (unless otherwise noted)


Based on information from JMA, the Tokyo VAAC reported that during 21-27 August explosions from Sakura-jima generated plumes that rose to altitudes of 1.2-3.4 km (4,000-11,000 ft) a.s.l. and drifted in multiple directions. During 24 and 26-27 August pilots observed ash plumes that rose to altitudes of 2.4-3 km (8,000-10,000 ft) a.s.l. and traveled SE and E. JMA reported that six explosions from Showa Crater during 23-26 August ejected tephra as far as 1,300 m. Incandescence from the crater was visible during 25-26 August.

Geologic Background. The Aira caldera in the northern half of Kagoshima Bay contains the post-caldera Sakurajima volcano, one of Japan's most active. Eruption of the voluminous Ito pyroclastic flow accompanied formation of the 17 x 23 km caldera about 22,000 years ago. The smaller Wakamiko caldera was formed during the early Holocene in the NE corner of the Aira caldera, along with several post-caldera cones. The construction of Sakurajima began about 13,000 years ago on the southern rim of Aira caldera and built an island that was finally joined to the Osumi Peninsula during the major explosive and effusive eruption of 1914. Activity at the Kitadake summit cone ended about 4850 years ago, after which eruptions took place at Minamidake. Frequent historical eruptions, recorded since the 8th century, have deposited ash on Kagoshima, one of Kyushu's largest cities, located across Kagoshima Bay only 8 km from the summit. The largest historical eruption took place during 1471-76.

Sources: Japan Meteorological Agency (JMA), Tokyo Volcanic Ash Advisory Center (VAAC)