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Jepang (diadministrasikan oleh Rusia) · Stratovolkan

Baransky

Sashiusudake [Baransky]

Tipe
Stratovolkan
Ketinggian
1128 m
Letusan terakhir
1951
Baransky
Foto: Витольд Муратов · CC BY-SA 3.0 · Wikimedia Commons
Tipe
Stratovolkan
Negara
Jepang (diadministrasikan oleh Rusia)
Wilayah
Pasifik Barat Laut / Kuril Volcanic Arc
Ketinggian
1128 m
Koordinat
45.104, 148.014
Letusan terakhir
1951
Kondisi tektonik
Zona subduksi / Kerak menengah (15-25 km)
Bentuk lahan
Komposit
Batuan utama
Andesit / Andesit basaltik
Ringkasan geologi

The Sashiusudake (also known as Baransky) volcanic complex along the Pacific coast in the central part of Iturup Island consists of a Holocene stratovolcano built over an eroded Pleistocene edifice. 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 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 Inggris

Baransky is a stratovolcano located in the central part of Iturup Island, Kuril Islands, Russia.

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Riwayat letusan

3 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu · Gunakan tombol panah untuk berpindah batang, Enter untuk membuka
1460~1509 · 1 letusan · VEI maks. ?1558~1607 · 1 letusan · VEI maks. ?1902~1951 · 1 letusan · VEI maks. 114601558170618041902

Garis waktu rinci

  1. 1951VEI 1Teramati
    1951-07-15 – akhir tidak diketahui
  2. 1570 (±30 tahun)VEI ?Perkiraan geologi
    1570 – akhir tidak diketahui
  3. 1460 (±30 tahun)VEI ?Perkiraan geologi
    1460 – akhir tidak diketahui

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