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Barkhatnaya

Barkhatnaya Sopka

화산대지 · Russia · 874m

The Holocene scoria cones of Barkhatnaya Sopka are located on a plateau 13 km N of Vilyuchik volcano on an uplifted eroded Miocene-Pliocene block. In this view looking NE, the Mt. Barkhatnaya cone which formed 3,000-4,000 years ago is to the left, and the reddish hill to the right is an early Holocene scoria cone. The white hill in the center is a part of an eroded rhyolitic body.
The Holocene scoria cones of Barkhatnaya Sopka are located on a plateau 13 km N of Vilyuchik volcano on an uplifted eroded Miocene-Pliocene block. In this view looking NE, the Mt. Barkhatnaya cone which formed 3,000-4,000 years ago is to the left, and the reddish hill to the right is an early Holocene scoria cone. The white hill in the center is a part of an eroded rhyolitic body. · 사진: Coyrighted photo by Oleg Dirksen (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
화산 유형
화산대지
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
해발
874m
좌표
52.802, 158.240
마지막 분화
-3550년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Cluster
주요 암석
Basalt / Picro-Basalt
지질학적 요약

The Barkhatnaya Sopka group of Pleistocene andesitic-to-rhyolitic lava domes and Holocene basaltic pyroclastic cones is located along the Paratunka River about 30 km NNW of Gorely volcano. The cinder cones are sitting on an uplifted block of eroded Miocene-Pliocene rocks. Most of the younger cones lie on the S and SE sides of the volcanic field. The Barkhatnaya cinder cone formed about 3,000-4,000 years ago (Ponomareva, 1992 p.c.).

Wikipedia 요약

영어 요약

Barkhatnaya Sopka is a volcano located in the southern part of Kamchatka Peninsula, Russia, along the Paratunka River. The mountain complex is named by the red-velvety color of its volcanic deposits.

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분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
3550 BCE~3550 BCE · 1건 · 최고 VEI ?3550 BCE3550 BCE3549 BCE3549 BCE3549 BCE

상세 타임라인

  1. 기원전 3550년VEI ?지질학적 추정
    BCE 3550 ~ 진행 중

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