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Cobb Segment

Fissure vent · Canada · 2100m (submarine)

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Type
Fissure vent
Country
Canada
Region
Eastern Pacific Volcanic Regions / Northeast Pacific Rifts Volcanic Province
Elevation
2100m (submarine)
Coordinates
46.880, -129.330
Last eruption
-1180
Tectonic setting
Rift zone / Oceanic crust (< 15 km)
Landform
Cluster
Major rock type
Basalt / Picro-Basalt
Geological summary

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.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1180 BCE~1180 BCE · 1 eruptions · max VEI ?1180 BCE1180 BCE1179 BCE1179 BCE1179 BCE

Detailed timeline

  1. 1180 BCEVEI ?Geological estimate
    BCE 1180 – Ongoing

External links

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