Bolshoy Kekuknaysky Volcano
Bolshoi-Kekuknaysky
순상화산 · Russia · 1401m

- 화산 유형
- 순상화산
- 국가
- Russia
- 지역
- Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
- 해발
- 1401m
- 좌표
- 56.483, 157.917
- 마지막 분화
- -5310년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Shield
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Bolshoi (Bolshoy) and Kekuknaysky are two large, partially overlapping basaltic shield volcanoes located NW and NNW, respectively, of Uksichan volcano. The massive Pleistocene shield volcanoes were constructed west of the axis of the Sredinny Range. Hawaiian-type calderas are located at the summits, and their flanks have numerous youthful cinder cones. The summit caldera of Bolshoi is breached by four radial valleys, whereas the 6-km-wide caldera of Kekuknaysky (also known as Leningradets volcano) is breached to the north. Young cinder cones and lava flows are particularly abundant on the NE flank of Kekuknaysky. Kekuk crater on the lower N flank erupted about 7,200 years ago.
Wikipedia 요약
영어 요약Bolshoy Kekuknaysky is a volcano located in the central part of the Kamchatka Peninsula, Russia. It comprises two shield volcanoes: Bolshoy (1301 m) and Kekuknaysky (1401 m). Their lava flows and cinder cones have dammed a valley dissecting the mountain, creating the Bolshoye Goltsovoye and Maloye Goltsovoe lakes. The last eruption occurred at Kekuk Crater, about 7,200 years ago.
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분화 이력
상세 타임라인
- 기원전 5310년 (±100년)VEI 3지질학적 추정BCE 5310 ~ 진행 중N flank of Kekuknaysky (Kekuk Crater)
외부 링크
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