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Oshima Ōshima

Oshima-Oshima

Estratovolcán · Japan · 732 m

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. · Foto: 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
Tipo
Estratovolcán
País
Japan
Región
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Altitud
732 m
Coordenadas
41.510, 139.367
Última erupción
1790
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

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.

Resumen de Wikipedia

Ōshima es una isla deshabitada en el mar de Japón, localizada 50 kilómetros al oeste de la villa de Matsumae y, por lo tanto, el punto más occidental de Hokkaidō. Forma parte de Matsumae en la subprefectura de Oshima, prefectura de Hokkaidō, Japón. Para distinguirla de otras islas con el mismo nombre, a veces se le conoce con el nombre de Oshima Ōshima o Matsumae Ōshima .

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
800 BCE~601 BCE · 1 erupciones · VEI máx. ?196~395 · 1 erupciones · VEI máx. ?1591~1790 · 4 erupciones · VEI máx. 4800 BCE202 BCE3959931591

Línea de tiempo detallada

  1. 1790VEI 2Observado
    1790-01 – En curso
    Nishi-yama
  2. 1786VEI 2Estimación geológica
    1786 – En curso
    Nishi-yama
  3. 1759VEI 2Observado
    1759-08-19 – En curso
    Nishi-yama
  4. 1741VEI 4Observado
    1741-08-18 – 1742-05
    Nishi-yama
  5. 250 (±150 años)VEI ?Estimación geológica
    250 – En curso
    Nishi-yama
  6. 800 a. C. (±100 años)VEI ?Estimación geológica
    BCE 800 – En curso
    Nishi-yama

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.