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Cobb Segment

Fisura volcánica · Canada · 2100 m (submarino)

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Tipo
Fisura volcánica
País
Canada
Región
Eastern Pacific Volcanic Regions / 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.

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

⚠ Solo como referencia. No apto para respuesta ante emergencias.