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Bogdan Khmelnitsky

Chirippusan [Chirip]

성층화산 · Japan - administered by Russia · 1587m

The Chirippusan Peninsula protrudes NW into the Sea of Okhotsk from central Iturup Island and is composed of two Holocene cones. Minamichirippusan (center) lies at the southern end of the peninsula and Chirippusan (in the background to the left) forms the northern end. Lava flows from Minamichirippusan reach the coast on both the E and W sides of the peninsula.
The Chirippusan Peninsula protrudes NW into the Sea of Okhotsk from central Iturup Island and is composed of two Holocene cones. Minamichirippusan (center) lies at the southern end of the peninsula and Chirippusan (in the background to the left) forms the northern end. Lava flows from Minamichirippusan reach the coast on both the E and W sides of the peninsula. · 사진: Photo by Alexander Rybin, 2001 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin). · Wikimedia Commons
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

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1843~1845 · 1건 · 최고 VEI 21858~1860 · 1건 · 최고 VEI 118431846185218551858

상세 타임라인

  1. 1860년VEI 1관측 기록
    1860 ~ 진행 중
    SE of Bogdan Khmelinitskii summit
  2. 1843년VEI 2관측 기록
    1843 ~ 진행 중

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