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Ostry

성층화산 · Russia · 2552m

Snow-capped Ostry is seen here from the NW. On the right horizon is an unnamed cone on the SW flank of Ostry, which erupted about 4,000 years ago producing a basaltic lava flow.
Snow-capped Ostry is seen here from the NW. On the right horizon is an unnamed cone on the SW flank of Ostry, which erupted about 4,000 years ago producing a basaltic lava flow. · 사진: Copyrighted photo by Maria Pevzner, 2005 (Russian Academy of Sciences, Moscow). · Wikimedia Commons
화산 유형
성층화산
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
해발
2552m
좌표
58.180, 160.820
마지막 분화
-2050년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Basalt / Picro-Basalt
지질학적 요약

Conical Ostry volcano (also known as Ostraya) is a late-Quaternary stratovolcano on the western side of the major NE-trending graben along the axis of the northern Sredinny Range. An unnamed cinder cone on the SW flank, informally referred to as "Cone X," erupted about 4,000 years ago, producing a basaltic lava flow.

Wikipedia 요약

영어 요약

Ostry is a stratovolcano located in the northern part of the Kamchatka Peninsula, Russia. It comprises the higher Ostry volcano and the smaller Kutina volcano. Ostry is one of the highest peaks of Sredinny Range.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
2050 BCE~2050 BCE · 1건 · 최고 VEI ?2050 BCE2050 BCE2049 BCE2049 BCE2049 BCE

상세 타임라인

  1. 기원전 2050년VEI ?지질학적 추정
    BCE 2050 ~ 진행 중
    SW flank cinder cone

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