본문으로 건너뛰기

Bolshoy Kekuknaysky Volcano

Bolshoi-Kekuknaysky

순상화산 · Russia · 1401m

Kekuk crater on the lower northern flank of the Bolshoi-Kekuknaysky volcanic complex formed about 7,200 years ago. The 1-km-wide crater formed beside a lava dome (left) which likely was erupted immediately prior to formation of the crater. Bolshoi and Kekuknaysky are two large partially overlapping Pleistocene edifices that contain scoria cones on their flanks.
Kekuk crater on the lower northern flank of the Bolshoi-Kekuknaysky volcanic complex formed about 7,200 years ago. The 1-km-wide crater formed beside a lava dome (left) which likely was erupted immediately prior to formation of the crater. Bolshoi and Kekuknaysky are two large partially overlapping Pleistocene edifices that contain scoria cones on their flanks. · 사진: Copyrighted photo by Adam Kirilenko, 2003.
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 요약

Bolshoy 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.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
5310 BCE~5310 BCE · 1건 · 최고 VEI 35310 BCE5310 BCE5309 BCE5309 BCE5309 BCE

상세 타임라인

  1. 기원전 5310년 (±100년)VEI 3지질학적 추정
    BCE 5310 ~ 진행 중
    N flank of Kekuknaysky (Kekuk Crater)

외부 링크

⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.