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Cobb Segment

Fisura volcánica · Canada · 2100 m (submarino)

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Tipo
Fisura volcánica
País
Canada
Región
Pacífico Oriental / Northeast Pacific Rifts Volcanic Province
Altitud
2100 m (submarino)
Coordenadas
46.880, -129.330
Última erupción
-1180
Contexto tectónico
Rift zone / Oceanic crust (< 15 km)
Forma volcánica
Cluster
Roca principal
Basalt / Picro-Basalt
Resumen geológico

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.

Resumen de Wikipedia

Resumen en inglés

Cobb 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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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1180 BCE~1180 BCE · 1 erupciones · VEI máx. ?1180 BCE1180 BCE1179 BCE1179 BCE1179 BCE

Línea de tiempo detallada

  1. 1180 a. C.VEI ?Estimación geológica
    BCE 1180 – En curso

Enlaces externos

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