Baransky
Sashiusudake [Baransky]
Stratovolkan · Japan - administered by Russia · 1107 m

- Tipe
- Stratovolkan
- Negara
- Japan - administered by Russia
- Wilayah
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Ketinggian
- 1107 m
- Koordinat
- 45.103, 148.015
- Letusan terakhir
- 1951
- Kondisi tektonik
- Subduction zone / Intermediate crust (15-25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
The Sashiusudake (also known as Baransky) volcanic complex along the Pacific coast in the central part of Iturup Island consists of an eroded Pleistocene volcano that is capped by a Holocene stratovolcano. A young summit lava dome is cut by a NW-trending chain of small explosion craters. A group of flank cones farther to the NW with a similar NW-SE orientation is partially surrounded by lava flows from the central crater of the andesitic-dacitic volcano. Lava flows from descended 4-5 km SE to reach the Pacific Ocean along a broad front. The only observed eruption occurred in 1951, when local inhabitants reported weak explosive activity at the summit. Strong solfataric activity continues from the summit and several flank craters, and the SW flank geothermal field contains hot springs and geysers. A small hydrothermal explosion took place in 1992 at an exploratory well in the SW-flank geothermal field.
Ringkasan Wikipedia
Ringkasan InggrisBaransky is a stratovolcano located in the central part of Iturup Island, Kuril Islands, Russia.
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Riwayat letusan
Garis waktu rinci
- 1951VEI 1Teramati1951-07-15 – Berlangsung
- 1570 (±30 tahun)VEI ?Perkiraan geologi1570 – Berlangsung
- 1460 (±30 tahun)VEI ?Perkiraan geologi1460 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.