Oshima Ōshima
Oshima-Oshima
Stratovulcano · Japan · 732 m

- Tipo
- Stratovulcano
- Paese
- Japan
- Regione
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- Altitudine
- 732 m
- Coordinate
- 41.510, 139.367
- Ultima eruzione
- 1790
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in ingleseŌshima 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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Storia delle eruzioni
Cronologia dettagliata
- 1790VEI 2Osservata1790-01 – In corsoNishi-yama
- 1786VEI 2Stima geologica1786 – In corsoNishi-yama
- 1759VEI 2Osservata1759-08-19 – In corsoNishi-yama
- 1741VEI 4Osservata1741-08-18 – 1742-05Nishi-yama
- 250 (±150 anni)VEI ?Stima geologica250 – In corsoNishi-yama
- 800 a.C. (±100 anni)VEI ?Stima geologicaBCE 800 – In corsoNishi-yama
Link esterni
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