Hakkōda Mountains
Hakkodasan
성층화산 · Japan · 1585m

- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- 해발
- 1585m
- 좌표
- 40.659, 140.877
- 마지막 분화
- 1550년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The basaltic-to-rhyolitic Hakkodasan volcano 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 than the southern group. Hakkoda-Odake, Ido-dake, and Tsurugi-dake have well-preserved craters. Akakuradake has a 1-km-wide explosion crater breached to the north. No historical eruptions are known, although an active solfatara occurs at Idodake, and hot springs are found at several locations within the caldera. Three minor phreatic eruptions were documented from Jigokunuma on the SW flank of Odake volcano from the 13th-17th centuries. Three soldiers on a training mission in July 1997 were killed by inhalation of volcanic gas.
Wikipedia 요약
영어 요약The 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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분화 이력
상세 타임라인
- 1550년 (±100년)VEI 1지질학적 추정1550 ~ 진행 중SW flank of O-dake (Jigoku-numa)
- 1340년 (±75년)VEI 1지질학적 추정1340 ~ 진행 중SW flank of O-dake (Jigoku-numa)
- 450년VEI 1지질학적 추정450 ~ 진행 중O-dake
- 기원전 50년VEI 1지질학적 추정BCE 50 ~ 진행 중O-dake
- 기원전 1150년VEI 1지질학적 추정BCE 1150 ~ 진행 중O-dake
- 기원전 2250년VEI 3지질학적 추정BCE 2250 ~ 진행 중O-dake
- 기원전 2850년VEI 2지질학적 추정BCE 2850 ~ 진행 중O-dake
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