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Matsumae Oshima

Oshima-Oshima

Stratovolkan · Japan · 732 m

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. · Foto: 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
Tipe
Stratovolkan
Negara
Japan
Wilayah
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Ketinggian
732 m
Koordinat
41.510, 139.367
Letusan terakhir
1790
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

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.

Ringkasan Wikipedia

Matsumae Ōshima atau hanya disebut sebagai Ōshima adalah sebuah pulau vulkanis tak berpenghuni di Laut Jepang, 50 kilometer (31 mi) ke arah barat dari kotapraja Matsumae dan merupakan titik paling barat Hokkaido. Secara administrasi, pulau ini adalah bagian dari Subprefektur Oshima di Hokkaido, Jepang. Untuk membedakan Ōshima dari pulau lain dengan nama yang sama, terkadang dikenal sebagai Oshima Ōshima .

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
800 BCE~601 BCE · 1 letusan · VEI maks. ?196~395 · 1 letusan · VEI maks. ?1591~1790 · 4 letusan · VEI maks. 4800 BCE202 BCE3959931591

Garis waktu rinci

  1. 1790VEI 2Teramati
    1790-01 – Berlangsung
    Nishi-yama
  2. 1786VEI 2Perkiraan geologi
    1786 – Berlangsung
    Nishi-yama
  3. 1759VEI 2Teramati
    1759-08-19 – Berlangsung
    Nishi-yama
  4. 1741VEI 4Teramati
    1741-08-18 – 1742-05
    Nishi-yama
  5. 250 (±150 tahun)VEI ?Perkiraan geologi
    250 – Berlangsung
    Nishi-yama
  6. 800 SM (±100 tahun)VEI ?Perkiraan geologi
    BCE 800 – Berlangsung
    Nishi-yama

Tautan eksternal

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