Tori-shima
Izu-Torishima
Stratovolcano · Japan · 394m

- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific Volcanic Regions / Izu Volcanic Arc
- Elevation
- 394m
- Coordinates
- 30.484, 140.303
- Last eruption
- 2002
- Tectonic setting
- Subduction zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Basalt / Picro-Basalt
Geological summary
The circular, 2.7-km-wide island of Izu-Torishima in the southern Izu Islands is capped by an unvegetated summit cone formed during an eruption in 1939. Fresh lava flows from this eruption form part of the northern coastline of the basaltic-to-dacitic edifice. The volcano is referred to as Izu-Torishima to distinguish it from the several other Japanese island volcanoes called Torishima ("Bird Island"). The main cone is truncated by a 1.5-km-wide caldera that contains two central cones, of which Ioyama is the highest. Historical eruptions have also occurred from flank vents near the north coast and offshore submarine vents. A submarine caldera 6-8 km wide lies immediately to the north.
From Wikipedia
Tori-shima 'Bird Island', or Izu-Torishima 'Bird Island of Izu Province') is an uninhabited Japanese island in the Pacific Ocean. The volcanic island is part of the Izu Islands.
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Eruption history
Detailed timeline
- 2013VEI 2Observed2013-07-06 – 2013-07-06
- 2002VEI 2Observed2002-08-12 – 2002-08-20Iwo-yama
- 1975VEI 2Observed1975-10-02 – Ongoing9 km S of Torishima
- 1965VEI 0Observed1965-11-13 – 1965-12-05
- 1939VEI 3Observed1939-08-17 – 1939-12-26North side of 1902 crater (Iwo-yama)
- 1902VEI 3Observed1902-08-07 – 1902-08-24Komochi-yama, N & SW offshore flanks
- 1871VEI 0Observed1871-04 – Ongoing
External links
⚠ For reference only. Not for emergency response.