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Cobb Segment

Fissure vent · Canada · 2100m (submarine)

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Type
Fissure vent
Country
Canada
Region
Eastern Pacific / 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.

From Wikipedia

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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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

⚠ For reference only. Not for emergency response.