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Oshima Ōshima

Oshima-Oshima

Stratovolcano · 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. · Photo: 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
Type
Stratovolcano
Country
Japan
Region
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Elevation
732m
Coordinates
41.510, 139.367
Last eruption
1790
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Basalt / Picro-Basalt
Geological summary

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.

From Wikipedia

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).

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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
800 BCE~601 BCE · 1 eruptions · max VEI ?196~395 · 1 eruptions · max VEI ?1591~1790 · 4 eruptions · max VEI 4800 BCE202 BCE3959931591

Detailed timeline

  1. 1790VEI 2Observed
    1790-01 – Ongoing
    Nishi-yama
  2. 1786VEI 2Geological estimate
    1786 – Ongoing
    Nishi-yama
  3. 1759VEI 2Observed
    1759-08-19 – Ongoing
    Nishi-yama
  4. 1741VEI 4Observed
    1741-08-18 – 1742-05
    Nishi-yama
  5. 250 (±150 yrs)VEI ?Geological estimate
    250 – Ongoing
    Nishi-yama
  6. 800 BCE (±100 yrs)VEI ?Geological estimate
    BCE 800 – Ongoing
    Nishi-yama

External links

⚠ For reference only. Not for emergency response.