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Spokoyny

Spokoiny

성층화산 · Russia · 2171m

Spokoiny, seen here from the east, lies immediately south of Ostry and NE of Iktunup volcano in the northern Sredinny Range. Lava flows from the summit cone extend down drainages to the east and west.
Spokoiny, seen here from the east, lies immediately south of Ostry and NE of Iktunup volcano in the northern Sredinny Range. Lava flows from the summit cone extend down drainages to the east and west. · 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
2171m
좌표
58.130, 160.820
마지막 분화
-3450년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Dacite
지질학적 요약

The dacitic-to-rhyolitic Spokoiny stratovolcano lies immediately south of Ostry volcano and NE of Iktunup volcano in the northern Sredinny Range. The volcano, also known as Kutina, was active during the early and mid-Holocene. Deposits from five eruptions during this interval have been documented, the last of which took place about 5400 years ago. Cinder cones are located on the W flank, and lava flows from the symmetrical summit cone extend down drainages to both the east and west.

Wikipedia 요약

영어 요약

Spokoyny is a stratovolcano in the northern part of the Sredinny Range in Russia's Kamchatka Peninsula. It forms part of the Volcanoes of Kamchatka Unesco world heritage site.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
3450 BCE~3450 BCE · 1건 · 최고 VEI ?3450 BCE3450 BCE3449 BCE3449 BCE3449 BCE

상세 타임라인

  1. 기원전 3450년VEI ?지질학적 추정
    BCE 3450 ~ 진행 중

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