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Vilyuchik

Vilyuchinsky

성층화산 · Russia · 2173m

Vilyuchik is a Holocene volcano that forms a prominent landmark south of Avachinsky Bay. It is seen here from the south between Mutnovsky and Gorely volcanoes. Deep erosional valleys are visible on the flanks, and lava domes scoria cones were constructed at its base.
Vilyuchik is a Holocene volcano that forms a prominent landmark south of Avachinsky Bay. It is seen here from the south between Mutnovsky and Gorely volcanoes. Deep erosional valleys are visible on the flanks, and lava domes scoria cones were constructed at its base. · 사진: Photo by Phil Austin, University of Southern Florida, 1992 (courtesy of Pavel Kepezhinskas). · Wikimedia Commons
화산 유형
성층화산
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
해발
2173m
좌표
52.700, 158.280
마지막 분화
-8050년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

Vilyuchinsky, or Vilyuchik, is a steep-sided Pleistocene-to-Holocene stratovolcano south of Avachinsky Bay. Deep erosional gullies dissect the flanks, with Lava domes and young basaltic cinder cones at its base. Most of the growth of the volcano took place during the late Pleistocene. The last significant eruption took place from the summit crater about 10,000 years ago, producing a moderate airfall deposit and a lava flow. Landslides and rock avalanches have affected habited areas.

Wikipedia 요약

영어 요약

Vilyuchik, also known as Vilyuchinsky is a dormant stratovolcano in the southern part of the Kamchatka Peninsula, Russia. It is located about 30 kilometres (19 mi) SSW of the closed city of Vilyuchinsk.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
8050 BCE~8050 BCE · 1건 · 최고 VEI 28050 BCE8050 BCE8049 BCE8049 BCE8049 BCE

상세 타임라인

  1. 기원전 8050년VEI 2지질학적 추정
    BCE 8050 ~ 진행 중

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