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渡島大島

Oshima-Oshima

成層火山 · 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. · 写真: 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
タイプ
成層火山
Japan
地域
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
標高
732m
座標
41.510, 139.367
最終噴火
1790年
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Basalt / Picro-Basalt
地質学的概要

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 の要約

渡島大島(おしまおおしま)は、北海道松前郡松前町に属する無人島である。松前大島(まつまえおおしま)とも呼ばれる。松前町西方沖50kmの地点に位置する。大島の名は渡島小島に対してのもの。住所は全域にわたって松前郡松前町大島。

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噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
800 BCE~601 BCE · 1件 · 最大 VEI ?196~395 · 1件 · 最大 VEI ?1591~1790 · 4件 · 最大 VEI 4800 BCE202 BCE3959931591

詳細タイムライン

  1. 1790年VEI 2観測記録
    1790-01 ~ 進行中
    Nishi-yama
  2. 1786年VEI 2地質学的推定
    1786 ~ 進行中
    Nishi-yama
  3. 1759年VEI 2観測記録
    1759-08-19 ~ 進行中
    Nishi-yama
  4. 1741年VEI 4観測記録
    1741-08-18 ~ 1742-05
    Nishi-yama
  5. 250年 (±150年)VEI ?地質学的推定
    250 ~ 進行中
    Nishi-yama
  6. 紀元前 800年 (±100年)VEI ?地質学的推定
    BCE 800 ~ 進行中
    Nishi-yama

外部リンク

⚠ 参考情報です。緊急対応には使用しないでください。