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핫코다산

Hakkodasan

성층화산 · Japan · 1584m

Hakkoda consists of a group of 14 cones 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 the caldera floor to the NE of the Hakkoda group volcanoes, which bury the SE caldera wall. This view looks from the W towards the northern Akakuradake, Idodake, and Hakkodasan volcanoes seen from left to right.
Hakkoda consists of a group of 14 cones 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 the caldera floor to the NE of the Hakkoda group volcanoes, which bury the SE caldera wall. This view looks from the W towards the northern Akakuradake, Idodake, and Hakkodasan volcanoes seen from left to right. · 사진: Photo by Takashi Kudo, 1996 (Hokkaido University). · Wikimedia Commons
화산 유형
성층화산
국가
Japan
지역
북서태평양 / Northeast Japan Volcanic Arc
해발
1584m
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 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.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
2850 BCE~2650 BCE · 1건 · 최고 VEI 22250 BCE~2050 BCE · 1건 · 최고 VEI 31250 BCE~1050 BCE · 1건 · 최고 VEI 150 BCE~150 · 1건 · 최고 VEI 1350~550 · 1건 · 최고 VEI 11150~1350 · 1건 · 최고 VEI 11350~1550 · 1건 · 최고 VEI 12850 BCE1850 BCE650 BCE3501350

상세 타임라인

  1. 1550년 (±100년)VEI 1지질학적 추정
    1550 ~ 진행 중
    SW flank of O-dake (Jigoku-numa)
  2. 1340년 (±75년)VEI 1지질학적 추정
    1340 ~ 진행 중
    SW flank of O-dake (Jigoku-numa)
  3. 450년VEI 1지질학적 추정
    450 ~ 진행 중
    O-dake
  4. 기원전 50년VEI 1지질학적 추정
    BCE 50 ~ 진행 중
    O-dake
  5. 기원전 1150년VEI 1지질학적 추정
    BCE 1150 ~ 진행 중
    O-dake
  6. 기원전 2250년VEI 3지질학적 추정
    BCE 2250 ~ 진행 중
    O-dake
  7. 기원전 2850년VEI 2지질학적 추정
    BCE 2850 ~ 진행 중
    O-dake

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