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Cobb Segment

열극 분화구 · Canada · 2100m (해저)

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화산 유형
열극 분화구
국가
Canada
지역
Eastern Pacific Volcanic Regions / Northeast Pacific Rifts Volcanic Province
해발
2100m (해저)
좌표
46.880, -129.330
마지막 분화
-1180년
판구조 환경
Rift zone / Oceanic crust (< 15 km)
화산 지형
Cluster
주요 암석
Basalt / Picro-Basalt
지질학적 요약

The Cobb Segment is in the northern part of the Juan de Fuca Ridge, south of the Endeavour Ridge segment. This 150-km-long segment, also known as the Northern Symmetrical or NSymm Segment, is the longest of the Juan de Fuca Ridge. It has a narrow axial crest, 1-2 km wide, with a shallow graben that has a high point at about 2,300 m depth. A prominent seamount with hydrothermal deposits at its summit lies just west of the axis high and was the source of a broad area of young, mostly sediment-free lava flows. As with other Juan de Fuca Ridge segments, a shallow magma source is thought to underlie the Cobb Segment, and a preliminary Uranium-series date of Holocene age was obtained on a basaltic lava flow.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1180 BCE~1180 BCE · 1건 · 최고 VEI ?1180 BCE1180 BCE1179 BCE1179 BCE1179 BCE

상세 타임라인

  1. 기원전 1180년VEI ?지질학적 추정
    BCE 1180 ~ 진행 중

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