SUMMARY:Type: composite |
GEOLOGIC HISTORYThe Zao volcano group, the most active of northern Honshu, consists of a complex cluster of stratovolcanoes straddling the Pacific Ocean-Japan Sea divide. The Pleistocene Ryu-zan and Aoso volcanoes form the northern and southern Zao groups, respectively, NW and SE of the central Zao group. Zao volcano proper forms the central Zao group, a volcanic complex topped by several lava domes and the Goshiki-dake tuff cone. Goshiki-dake contains the active Okama crater, filled with a colorful crater lake. It has been the source of most of the frequent historical eruptions of Zao volcano. Historic Activity: More than 30 eruptions from the Zoa complex have been documented in the past 1200 years, the most recent an emission of fine sulfur in 1939-40. Recent Activity: A seismic shock of M 4.7 occurred on Sept. 1, 1992 a few kilometers ESE of the summit. Data Sources
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ADDITIONAL INFORMATION
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Last Update: 2/27/00 |