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Cobb Segment

Rekahan erupsi · Canada · 2100 m (bawah laut)

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Tipe
Rekahan erupsi
Negara
Canada
Wilayah
Eastern Pacific Volcanic Regions / 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.

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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