Cobb Segment
Fisura volcánica · Canada · 2100 m (submarino)
- Tipo
- Fisura volcánica
- País
- Canada
- Región
- Eastern Pacific Volcanic Regions / Northeast Pacific Rifts Volcanic Province
- Altitud
- 2100 m (submarino)
- Coordenadas
- 46.880, -129.330
- Última erupción
- -1180
- Contexto tectónico
- Rift zone / Oceanic crust (< 15 km)
- Forma volcánica
- Cluster
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
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.
Historial de erupciones
Línea de tiempo detallada
- 1180 a. C.VEI ?Estimación geológicaBCE 1180 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.