다이세쓰산
Taisetsuzan
성층화산 · Japan · 2291m

- 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 요약The 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.
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분화 이력
상세 타임라인
- 1739년VEI ?지질학적 추정1739 ~ 진행 중Asahi-dake
- 기원전 550년 (±500년)VEI ?지질학적 추정BCE 550 ~ 진행 중Asahi-dake
- 기원전 1450년 (±50년)VEI ?지질학적 추정BCE 1450 ~ 진행 중Asahi-dake
- 기원전 2800년 (±100년)VEI ?지질학적 추정BCE 2800 ~ 진행 중Asahi-dake
- 기원전 3200년 (±75년)VEI ?지질학적 추정BCE 3200 ~ 진행 중Asahi-dake
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