Japan · Stratovolcano
Oshima Ōshima
Oshima-Oshima
- Type
- Stratovolcano
- Elevation
- 732m
- Last eruption
- 1790

- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific / 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.
Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →
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).
Wikipedia · CC BY-SA · Read full article →
Eruption history
6 recordedGlossaryRecord summary
- Confirmed eruptions
- 5
- Uncertain eruptions
- 1
- Span of confirmed record
- 800 BCE (±100 yrs) – 1790
- Largest confirmed eruption
- VEI 4 (1741)
- Confirmed eruptions since 1900
- 0
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
Detailed timeline
- 1790VEI 2Observed1790-01 – end unknownNishi-yama
- 1786VEI 2Method not stated1786 – end unknownNishi-yama
- 1759VEI 2Observed1759-08-19 – end unknownNishi-yama
- 1741VEI 4Observed1741-08-18 – 1742-05Nishi-yama
- 250 (±150 yrs)VEI ?Geological estimate250 – end unknownNishi-yama
- 800 BCE (±100 yrs)VEI ?Geological estimate800 BCE – end unknownNishi-yama
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.