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Cobb Seamount

Cobb Segment

Frattura eruttiva · Canada · 2100 m (sottomarino)

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Tipo
Frattura eruttiva
Paese
Canada
Regione
Pacifico orientale / Northeast Pacific Rifts Volcanic Province
Altitudine
2100 m (sottomarino)
Coordinate
46.880, -129.330
Ultima eruzione
-1180
Contesto tettonico
Rift zone / Oceanic crust (< 15 km)
Forma vulcanica
Cluster
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1180 BCE~1180 BCE · 1 eruzioni · VEI max. ?1180 BCE1180 BCE1179 BCE1179 BCE1179 BCE

Cronologia dettagliata

  1. 1180 a.C.VEI ?Stima geologica
    BCE 1180 – In corso

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