SUMMARY:Type: composite |
GEOLOGIC HISTORYLocated on northern Honshu northwest of Morioka City, Iwate sits adjacent to an older cone. Viewed from the east, Iwate volcano has a symmetrical profile that invites comparison with Fuji, but on the west an older cone is visible containing an oval-shaped, 1.8 x 3 km caldera. After the growth of Nishi-Iwate volcano beginning about 700,000 years ago, activity migrated eastward to form Higashi-Iwate volcano. Iwate has collapsed seven times during the past 230,000 years, most recently between 739 and 1615 AD. The summit cone of Iwate volcano, Yakushi-dake, is truncated by a 500-m-wide crater. It rises well above and buries the eastern rim of the caldera, which is breached by a narrow gorge on the NW. A central cone containing a 500-m-wide crater partially filled by a lake is located in the center of the oval-shaped caldera. A young lava flow from Yakushi-dake descended into the caldera and a fresh-looking lava flow from the 1732 eruption traveled down the NE flank. Historic Activity:
Recent Activity:
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Last Update: 10/29/00 |