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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
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 요약

Ōshima 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).

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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