Cobb Segment
열극 분화구 · Canada · 2100m (해저)
- 화산 유형
- 열극 분화구
- 국가
- Canada
- 지역
- 동태평양 / 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.
Wikipedia 요약
영어 요약Cobb Seamount is a seamount and guyot located 500 km (310 mi) west of Grays Harbor, Washington, United States. Cobb Seamount is one of the seamounts in the Cobb–Eickelberg Seamount chain, a chain of underwater volcanoes created by the Cobb hotspot that terminates near the coast of Alaska. It lies just west of the Cascadia subduction zone, and was discovered in August 1950 by the U.S. Fish and Wildlife Service fisheries research vessel R/V John N. Cobb . By 1967, over 927 km (576 mi) of soundings and dozens of samples from the seamount had been collected.
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분화 이력
상세 타임라인
- 기원전 1180년VEI ?지질학적 추정BCE 1180 ~ 진행 중
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