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Report on Hakoneyama (Japan) — 13 May-19 May 2015

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 13 May-19 May 2015
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2015. Report on Hakoneyama (Japan). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 13 May-19 May 2015. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (13 May-19 May 2015)


Hakoneyama

Japan

35.233°N, 139.021°E; summit elev. 1438 m

All times are local (unless otherwise noted)


JMA reported that during 14-17 May seismicity at Hakoneyama remained high. Inclinometer data showed variations related to seismicity, and vigorous steaming from the hot springs was observed. The Alert Level remained at 2 (on a 5-level scale). According to a news article, the ground level in the Owakudani hot spring area had risen 12 cm during 17 April-15 May; the deformation occurred in an area 200 m in diameter. The article also noted that 471 earthquakes were recorded on 15 May, the highest number ever recorded there in one day.

Geologic Background. Hakoneyama volcano is truncated by two overlapping calderas, the largest of which is 10 x 11 km wide. The calderas were formed as a result of two major explosive eruptions about 180,000 and 49,000-60,000 years ago. Scenic Lake Ashi lies between the SW caldera wall and a half dozen post-caldera lava domes that were constructed along a NW-SE trend cutting through the center of the calderas. Dome growth occurred progressively to the NW, and the largest and youngest of these, Kamiyama, forms the high point. The calderas are breached to the east by the Hayakawa canyon. A phreatic explosion about 3000 years ago was followed by collapse of the NW side of Kamiyama, damming the Hayakawa valley and creating Lake Ashi. The latest magmatic eruptive activity about 2900 years ago produced a pyroclastic flow and a lava dome in the explosion crater, although phreatic eruptions took place as recently as the 12-13th centuries CE. Seismic swarms have occurred during the 20th century. Lake Ashi, along with the thermal areas in the caldera, is a popular resort destination SW of Tokyo.

Source: Japan Meteorological Agency (JMA)