Japan · Stratovolcano
Hakkōda Mountains
Hakkodasan
- Type
- Stratovolcano
- Elevation
- 1584m
- Last eruption
- 1550

- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific / Northeast Japan Volcanic Arc
- Elevation
- 1584m
- Coordinates
- 40.659, 140.877
- Last eruption
- 1550
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic andesite
Geological summary
The Hakkodasan complex includes at least 17 stratovolcanoes and lava domes south of Mutsu Bay at the northern end of Honshu. The NE rim of an 8-km-wide Pleistocene caldera forms an arcuate ridge across a flat caldera-floor moat NE of the Hakkoda group volcanoes, which bury the SE caldera wall. A northern group of volcanoes, constructed within the caldera, appears to be younger. The craters at Hakkoda-Odake, Ido-dake, and Tsurugi-dake appear morphologically young. Akakuradake has a 1-km-wide explosion crater breached to the north. An active solfatara occurs at Idodake, and hot springs are found at several locations within the caldera. Three minor phreatic events from Jigokunuma on the SW flank of Odake volcano produced tephra radiocarbon dated to the 13th-17th centuries. Three soldiers on a training mission in July 1997 were killed on the lower N flank of Hakkoda when they slipped into a depression containing a high percentage of CO2 gas wiht a magmatic origin.
From Wikipedia
The Hakkōda Mountains are an active volcanic complex in south-central Aomori Prefecture, Japan, in Towada-Hachimantai National Park. Often called Mount Hakkōda or simply Hakkōda (八甲田), the mountains are collectively listed as one of the 100 Famous Japanese Mountains. Its highest peak, Mount Ōdake, lies 21.3 kilometers (13.2 mi) southeast of central Aomori and 28 kilometers (17 mi) west of central Towada and has an elevation of 1,585 meters (5,200 ft). The Hakkōda Mountains are a part of the Ōu Mountains which make up part of the Northeastern Japan Arc, a segment of the Pacific Ring of Fire. The volcanic complex consists of fourteen stratovolcanoes and lava domes arranged into two volcanic groups. The Northern Hakkōda Volcanic Group emerges from the rim of an 8-kilometer-wide (5.0 mi) caldera that dates back to the Pleistocene. The Southern Hakkōda Volcanic Group predates the caldera.
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Eruption history
7 recordedGlossaryDetailed timeline
- 1550 (±100 yrs)VEI 1Geological estimate1550 – end unknownSW flank of O-dake (Jigoku-numa)
- 1340 (±75 yrs)VEI 1Geological estimate1340 – end unknownSW flank of O-dake (Jigoku-numa)
- 450VEI 1Geological estimate450 – end unknownO-dake
- 50 BCEVEI 1Geological estimate50 BCE – end unknownO-dake
- 1150 BCEVEI 1Geological estimate1150 BCE – end unknownO-dake
- 2250 BCEVEI 3Geological estimate2250 BCE – end unknownO-dake
- 2850 BCEVEI 2Geological estimate2850 BCE – end unknownO-dake
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.