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