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Cobb Segment

Rekahan erupsi · Canada · 2100 m (bawah laut)

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Tipe
Rekahan erupsi
Negara
Canada
Wilayah
Pasifik Timur / Northeast Pacific Rifts Volcanic Province
Ketinggian
2100 m (bawah laut)
Koordinat
46.880, -129.330
Letusan terakhir
-1180
Kondisi tektonik
Rift zone / Oceanic crust (< 15 km)
Bentuk lahan
Cluster
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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1180 BCE~1180 BCE · 1 letusan · VEI maks. ?1180 BCE1180 BCE1179 BCE1179 BCE1179 BCE

Garis waktu rinci

  1. 1180 SMVEI ?Perkiraan geologi
    BCE 1180 – Berlangsung

Tautan eksternal

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