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Komarov

성층화산 · Russia · 2065m

Hydrothermally altered rocks form the summit ridge of Komarov in this view from the east. Komarov is a complex structure in the northern half of the Gamchen ridge and lies at the western end of a 2.5 x 4 km caldera. Holocene lava flows, such as the one in the foreground, extend beyond the caldera to the east and west.
Hydrothermally altered rocks form the summit ridge of Komarov in this view from the east. Komarov is a complex structure in the northern half of the Gamchen ridge and lies at the western end of a 2.5 x 4 km caldera. Holocene lava flows, such as the one in the foreground, extend beyond the caldera to the east and west. · 사진: Copyrighted photo by Vera Ponomareva (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
화산 유형
성층화산
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
해발
2065m
좌표
55.033, 160.725
마지막 분화
950년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Basalt / Picro-Basalt
지질학적 요약

Komarov volcano is a complex structure along the Gamchen ridge. The summit area includes two irregular craters ~300m in diameter. Lengthy Holocene lava flows extend to the east and west. Growth began about 1,500 years ago following cessation of activity at Vysoky volcano. No reported eruptions are known, but the summit region has undergone extensive hydrothermal alteration, and fumarolic areas occur there and on the northern and southern flanks.

Wikipedia 요약

영어 요약

Komarov is an inactive stratovolcano located in the southeastern part of the Kamchatka Peninsula, Russia. It was named after Vladimir L. Komarov.

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분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
450~500 · 1건 · 최고 VEI 0900~950 · 1건 · 최고 VEI ?450550700800900

상세 타임라인

  1. 950년VEI ?지질학적 추정
    950 ~ 진행 중
  2. 450년VEI 0지질학적 추정
    450 ~ 진행 중

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