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Veer

화쇄구 · Russia · 520m

Flow ridges are visible on the surface of a sparsely vegetated lava flow originating from the Veer scoria cone to the right, in the Levaya Avacha river valley. Veer is one of a number of cones scattered throughout the Avacha river basin. This eruption took place 1,600-1,700 years Before Present (BP).
Flow ridges are visible on the surface of a sparsely vegetated lava flow originating from the Veer scoria cone to the right, in the Levaya Avacha river valley. Veer is one of a number of cones scattered throughout the Avacha river basin. This eruption took place 1,600-1,700 years Before Present (BP). · 사진: Copyrighted photo by Oleg Dirksen (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
화산 유형
화쇄구
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
해발
520m
좌표
53.752, 158.448
마지막 분화
390년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Minor (Basaltic)
주요 암석
Basalt / Picro-Basalt
지질학적 요약

Cinder cones along the Levaya Avacha River about 60 km N of Petropavlovsk-Kamchatskiy erupted lavas over young river terraces. The basaltic Veer cone, located on the W side of the river, produced a lava flow with prominent ridges that descended into the valley. Although Krijanovsky (1934) listed an 1856 eruption, stratigraphic studies have shown that the eruption occurred sometime between the 1,500 years before present (BP) eruption from Barany Amphitheater of Opala volcano and a 1,630 BP eruption from Avachinsky (Dirksen, 1999 pers. comm.). Nearby andesitic Pravy volcano is also of postglacial age.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
390~390 · 1건 · 최고 VEI 2390390391391391

상세 타임라인

  1. 390년 (±75년)VEI 2지질학적 추정
    390 ~ 진행 중

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