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다이세쓰산

Taisetsuzan

성층화산 · Japan · 2291m

Geothermal activity and recent craters occupy the western slope of Asahidake, one of the Daisetsu group volcanoes in central Hokkaido. Taisetsuzan is a complex group of cones and lava domes associated with a 2-km-wide caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW from the caldera center.
Geothermal activity and recent craters occupy the western slope of Asahidake, one of the Daisetsu group volcanoes in central Hokkaido. Taisetsuzan is a complex group of cones and lava domes associated with a 2-km-wide caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW from the caldera center. · 사진: Photo by Ichio Moriya, 1993 (Kanazawa University). · Wikimedia Commons
화산 유형
성층화산
국가
Japan
지역
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
해발
2291m
좌표
43.664, 142.854
마지막 분화
1739년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

The Taisetsuzan volcano group lies at the northern end of the Taisetsu-Tokachi graben in central Hokkaido. It consists of a complex of stratovolcanoes and lava domes associated with a 2-km-wide caldera. The eight satellitic volcanoes are aligned along a ring fracture that is centered over the eastern rim of the caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW of the center of the caldera. Other stratovolcanoes are located along a NE-SW line cutting through the caldera that trends toward the Tokachi volcano complex to the SW. In contrast to the Tokachi group, no historical eruptions are known, although the latest phreatic eruption took place sometime after 1739 CE. Fumarolic areas are located on Asahidake, where at one time sulfur was mined, and in the caldera.

Wikipedia 요약

영어 요약

The Daisetsuzan Volcanic Group is a volcanic group of peaks arranged around the 2 kilometres (1.2 mi) wide Ohachi-Daira caldera in Hokkaidō, Japan. In the Ainu language it is known as Nutapukaushipe, Nutaku Kamushupe, or Optateske. These peaks are the highest in Hokkaidō. The group lends its name to the Daisetsuzan National Park in which the volcanic group is located.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
3200 BCE~3002 BCE · 1건 · 최고 VEI ?2805 BCE~2607 BCE · 1건 · 최고 VEI ?1620 BCE~1422 BCE · 1건 · 최고 VEI ?632 BCE~434 BCE · 1건 · 최고 VEI ?1541~1739 · 1건 · 최고 VEI ?3200 BCE2015 BCE829 BCE3561541

상세 타임라인

  1. 1739년VEI ?지질학적 추정
    1739 ~ 진행 중
    Asahi-dake
  2. 기원전 550년 (±500년)VEI ?지질학적 추정
    BCE 550 ~ 진행 중
    Asahi-dake
  3. 기원전 1450년 (±50년)VEI ?지질학적 추정
    BCE 1450 ~ 진행 중
    Asahi-dake
  4. 기원전 2800년 (±100년)VEI ?지질학적 추정
    BCE 2800 ~ 진행 중
    Asahi-dake
  5. 기원전 3200년 (±75년)VEI ?지질학적 추정
    BCE 3200 ~ 진행 중
    Asahi-dake

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