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Cherpuk Group

화쇄구 · Russia · 1868m

The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range.
The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range. · 사진: Copyrighted photo by Adam Kirilenko, 2000 (Holocene Kamchatka Volcanoes, www.kamchatka.ginras.ru).
화산 유형
화쇄구
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
해발
1868m
좌표
55.550, 157.470
마지막 분화
-4550년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Minor
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky volcano that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that fed 1.8 km3 lava flows down both sides of the range to the NW and SE. A narrow tongue of the SE flow diverted an additional 10 km S, for a total distance of 22 km. Yuzhny Cherpuk, 11 km SSW of Ichinsky, produced a 1.7 km3 lava flow that traveled 18 km S and then SE. The flow descended to 640 m elevation and dammed tributaries of the Ketachan River, producing three lakes. The two cones are sometimes considered to be satellitic cones to Ichinsky, but Pevzner et al. (2000) noted petrological distinctions that suggest an independent origin. Unpublished radiocarbon ages revise those in Pevzner et al. (2000) and indicate that both cones were formed about 6,500 years ago.

Wikipedia 요약

영어 요약

Cherpuk Group is a group of two cinder cones located in the central part of Kamchatka Peninsula, Russia. It is a group of a few mostly dormant cinder cones.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
4550 BCE~4550 BCE · 1건 · 최고 VEI ?4550 BCE4550 BCE4549 BCE4549 BCE4549 BCE

상세 타임라인

  1. 기원전 4550년VEI ?지질학적 추정
    BCE 4550 ~ 진행 중
    North and South Cherpuk

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