Oshima Ōshima
Oshima-Oshima
Stratovolcano · Japan · 732m

- 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
Detailed timeline
- 1790VEI 2Observed1790-01 – OngoingNishi-yama
- 1786VEI 2Geological estimate1786 – OngoingNishi-yama
- 1759VEI 2Observed1759-08-19 – OngoingNishi-yama
- 1741VEI 4Observed1741-08-18 – 1742-05Nishi-yama
- 250 (±150 yrs)VEI ?Geological estimate250 – OngoingNishi-yama
- 800 BCE (±100 yrs)VEI ?Geological estimateBCE 800 – OngoingNishi-yama
External links
⚠ For reference only. Not for emergency response.