Cobb Segment
Fissure vent · Canada · 2100m (submarine)
- 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
Detailed timeline
- 1180 BCEVEI ?Geological estimateBCE 1180 – Ongoing
External links
⚠ For reference only. Not for emergency response.