오시마섬
Oshima-Oshima
성층화산 · Japan · 732m

- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- 북서태평양 / Northeast Japan Volcanic Arc
- 해발
- 732m
- 좌표
- 41.510, 139.367
- 마지막 분화
- 1790년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Oshima-Oshima, a 10 km2 island about 105 km W offshore from the SW tip of Hokkaido, is the emergent summit of two coalescing basaltic-to-andesitic stratovolcanoes. Higashiyama, at the east end of the island, is cut by a 2-km-wide caldera covered on its west side by Nishiyama volcano. The western cone failed during an eruption in 1741 CE, producing a mostly submarine debris avalanche that traveled 16 km and leaving a scarp open to the north. A tsunami associated with the collapse swept the coasts of Hokkaido, western Honshu, and Korea, and caused nearly 1,500 fatalities. The 1741 eruption concluded with the construction of a basaltic pyroclastic cone at the head of the amphitheater. No eruptions have occurred since the late-18th century.
Wikipedia 요약
영어 요약Ōshima is an uninhabited island in the Sea of Japan, 50 kilometers (31 mi) west of Matsumae town and therefore the westernmost point of Hokkaido. It is part of the town of Matsumae in Oshima Subprefecture in Hokkaido, Japan. To distinguish Ōshima from other islands with the same name, it is sometimes known as Oshima Ōshima (渡島大島) or Matsumae Ōshima (松前大島).
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분화 이력
상세 타임라인
- 1790년VEI 2관측 기록1790-01 ~ 진행 중Nishi-yama
- 1786년VEI 2지질학적 추정1786 ~ 진행 중Nishi-yama
- 1759년VEI 2관측 기록1759-08-19 ~ 진행 중Nishi-yama
- 1741년VEI 4관측 기록1741-08-18 ~ 1742-05Nishi-yama
- 250년 (±150년)VEI ?지질학적 추정250 ~ 진행 중Nishi-yama
- 기원전 800년 (±100년)VEI ?지질학적 추정BCE 800 ~ 진행 중Nishi-yama
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