Bogdan Khmelnitsky
Chirippusan [Chirip]
성층화산 · Japan - administered by Russia · 1587m
- 화산 유형
- 성층화산
- 국가
- Japan - administered by Russia
- 지역
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- 해발
- 1587m
- 좌표
- 45.338, 147.920
- 마지막 분화
- 1860년
- 판구조 환경
- Subduction zone / Intermediate crust (15-25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Chirippusan (also simply Chirip) volcano is on the Chirip Peninsula, which extends N into the Sea of Okhotsk from central Iturup Island. The summits of two overlapping stratovolcanoes are ~4.5 km apart along a volcanic ridge, with Kitachirippusan on the north and Minamichirippu (also called Bogdan Khmelnitskii) on the south. Lava flows from both edifices are truncated by a large 4-km-wide depression on the west side of the peninsula. Basaltic rocks dominate at both volcanoes over basaltic andesite and andesitic products. Kitachirippusan has a shallow summit crater, partially filled by a small lake, that has fed lava flows down all sides; satellitic cones are located on the northern flank. Lava flows from Minamichirippusan reach the coast on both the east and west. Only two eruptions are known, one in 1843 CE and another in 1860 CE from a vent SE of the Minamichirippusan summit.
분화 이력
상세 타임라인
- 1860년VEI 1관측 기록1860 ~ 진행 중SE of Bogdan Khmelinitskii summit
- 1843년VEI 2관측 기록1843 ~ 진행 중
외부 링크
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- 🔗 Smithsonian GVP 원본 페이지
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