SUMMARY:Type: composite |
GEOLOGIC HISTORYTokachi consists of a group of stratovolcanoes arranged on a NE-SW line above a plateau of welded Pleistocene tuffs. Numerous explosion craters and cinder cones are located on the upper flanks, with the youngest Holocene craters at the NW end of the chain. Historic Activity: At least 12 eruptions from 1670 to 1962. Partial cone collapse during a 1926 eruption produced a disastrous avalanche and mudflow. Recent Activity:
Data Sources
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ADDITIONAL INFORMATION
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Last Update: 2/26/00 |