Matsumae Oshima
Oshima-Oshima
Stratovolkan · Japan · 732 m

- Tipe
- Stratovolkan
- Negara
- Japan
- Wilayah
- Pasifik Barat Laut / 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
Ringkasan InggrisŌshima 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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Riwayat letusan
Garis waktu rinci
- 1790VEI 2Teramati1790-01 – BerlangsungNishi-yama
- 1786VEI 2Perkiraan geologi1786 – BerlangsungNishi-yama
- 1759VEI 2Teramati1759-08-19 – BerlangsungNishi-yama
- 1741VEI 4Teramati1741-08-18 – 1742-05Nishi-yama
- 250 (±150 tahun)VEI ?Perkiraan geologi250 – BerlangsungNishi-yama
- 800 SM (±100 tahun)VEI ?Perkiraan geologiBCE 800 – BerlangsungNishi-yama
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.