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

- 화산 유형
- 성층화산
- 국가
- Japan - administered by Russia
- 지역
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- 해발
- 1107m
- 좌표
- 45.103, 148.015
- 마지막 분화
- 1951년
- 판구조 환경
- Subduction zone / Intermediate crust (15-25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
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.
Wikipedia 요약
영어 요약Baransky is a stratovolcano located in the central part of Iturup Island, Kuril Islands, Russia.
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분화 이력
상세 타임라인
- 1951년VEI 1관측 기록1951-07-15 ~ 진행 중
- 1570년 (±30년)VEI ?지질학적 추정1570 ~ 진행 중
- 1460년 (±30년)VEI ?지질학적 추정1460 ~ 진행 중
외부 링크
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