Report on Aira (Japan) — 17 July-23 July 2013
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
17 July-23 July 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, 17 July-23 July 2013. Smithsonian Institution and US Geological Survey.
31.593°N, 130.657°E; summit elev. 1117 m
All times are local (unless otherwise noted)
JMA reported that five explosions at Sakura-jima's Showa Crater were detected during 16-19 July, and ejected tephra as far as 1.3 km. A large plume rose 3.5 km above the crater on 16 July. Incandescence from the crater was observed at night during 18-19 July. Based on information from JMA, the Tokyo VAAC reported that during 18-21 July explosions generated plumes that rose to altitudes of 2.4-4.3 km (8,000-14,000 ft) a.s.l. and drifted N, E, SE, and S. Ash was sometimes detected in satellite images. On 19 July a pilot observed an ash plume that rose to an altitude of 6.1 km (20,000 ft) a.s.l. and drifted SE.
Geological Summary. 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)