Cobb Segment
열극 분화구 · Canada · 2100m (해저)
- 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
상세 타임라인
- 기원전 1180년VEI ?지질학적 추정BCE 1180 ~ 진행 중
외부 링크
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