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오시마섬

Oshima-Oshima

성층화산 · Japan · 732m

Oshima-Oshima volcano is seen here from the N with the Kanpodake cone (back-center) that formed during the 1741 eruption. Major edifice collapse that year produced a large scarp open to the north, with the walls visible at the sides of the image. The 4-km-wide island is 55 km W of the SW tip of Hokkaido, and is the emergent summit of two coalescing volcanoes: Higashiyama at the eastern end of the island, and Nishiyama at the western end.
Oshima-Oshima volcano is seen here from the N with the Kanpodake cone (back-center) that formed during the 1741 eruption. Major edifice collapse that year produced a large scarp open to the north, with the walls visible at the sides of the image. The 4-km-wide island is 55 km W of the SW tip of Hokkaido, and is the emergent summit of two coalescing volcanoes: Higashiyama at the eastern end of the island, and Nishiyama at the western end. · 사진: Copyrighted photo by Tomoyo Hayakawa (Japanese Quaternary Volcanoes database, RIODB, http://riodb02.ibase.aist.go.jp/strata/VOL_JP/EN/index.htm and Geol Surv Japan, AIST, http://www.gsj.jp/). · Wikimedia Commons
화산 유형
성층화산
국가
Japan
지역
Northwestern Pacific Volcanic Regions / 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

요약이 짧습니다. 자세한 내용은 전체 기사를 확인하세요.

오시마섬(일본어: 渡島大島)는 홋카이도 마쓰마에군 마쓰마에정 해역에 있는 섬이다.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
800 BCE~601 BCE · 1건 · 최고 VEI ?196~395 · 1건 · 최고 VEI ?1591~1790 · 4건 · 최고 VEI 4800 BCE202 BCE3959931591

상세 타임라인

  1. 1790년VEI 2관측 기록
    1790-01 ~ 진행 중
    Nishi-yama
  2. 1786년VEI 2지질학적 추정
    1786 ~ 진행 중
    Nishi-yama
  3. 1759년VEI 2관측 기록
    1759-08-19 ~ 진행 중
    Nishi-yama
  4. 1741년VEI 4관측 기록
    1741-08-18 ~ 1742-05
    Nishi-yama
  5. 250년 (±150년)VEI ?지질학적 추정
    250 ~ 진행 중
    Nishi-yama
  6. 기원전 800년 (±100년)VEI ?지질학적 추정
    BCE 800 ~ 진행 중
    Nishi-yama

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