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

- Type
- Stratovolcano
- Country
- Japan - administered by Russia
- Region
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Elevation
- 1107m
- Coordinates
- 45.103, 148.015
- Last eruption
- 1951
- Tectonic setting
- Subduction zone / Intermediate crust (15-25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
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.
From Wikipedia
Baransky is a stratovolcano located in the central part of Iturup Island, Kuril Islands, Russia.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 1951VEI 1Observed1951-07-15 – Ongoing
- 1570 (±30 yrs)VEI ?Geological estimate1570 – Ongoing
- 1460 (±30 yrs)VEI ?Geological estimate1460 – Ongoing
External links
⚠ For reference only. Not for emergency response.