SUMMARY:Type: composite |
GEOLOGIC HISTORYHakkoda, Å20 km SE of Aomori City, consits of stratocones and lava domes; the highest peak is O-take (1,585 m). After the formation of the Minami (S)-Hakkoda volcanic group (basalt, 3.9-0.5 Ma), the Kakkoda caldera was created due to a large-scale pyroclastic-flow eruption (dacite, 1-0.8 Ma), followed by the formation of the Kita (N)-Hakkoda volcano group (mainly andesite, 1-0.3 Ma). Historic Activity: There are strong solfataras around O-take, but there is no record of any historical eruptions. Recent Activity: On July 14, 1997 a group of Japanese troops on a training mission were over come by gases in a depression, three died. Data Sources
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ADDITIONAL INFORMATION
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Last Update: 2/27/00 |