Cobb Seamount
Cobb Segment
Frattura eruttiva · Canada · 2100 m (sottomarino)
- Tipo
- Frattura eruttiva
- Paese
- Canada
- Regione
- Eastern Pacific Volcanic Regions / Northeast Pacific Rifts Volcanic Province
- Altitudine
- 2100 m (sottomarino)
- Coordinate
- 46.880, -129.330
- Ultima eruzione
- -1180
- Contesto tettonico
- Rift zone / Oceanic crust (< 15 km)
- Forma vulcanica
- Cluster
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
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.
Sintesi da Wikipedia
Il Cobb Seamount è una montagna sottomarina, e più precisamente un vulcano sottomarino con la forma troncoconica tipica del guyot, situato circa 500 km a ovest di Grays Harbor, nello Stato di Washington degli Stati Uniti d'America.
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Storia delle eruzioni
Cronologia dettagliata
- 1180 a.C.VEI ?Stima geologicaBCE 1180 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.