Vilyuchik
Vilyuchinsky
성층화산 · Russia · 2173m

- 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 요약Vilyuchik, 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.
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분화 이력
상세 타임라인
- 기원전 8050년VEI 2지질학적 추정BCE 8050 ~ 진행 중
외부 링크
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