Cobb Seamount (original) (raw)

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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 , nello Stato di Washington degli Stati Uniti d'America.

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dbo:abstract Cobb Seamount is a seamount (underwater volcano) 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 (FWS 1601). By 1967, over 927 km (576 mi) of soundings and dozens of samples from the seamount had been collected. Cobb Seamount is geologically interesting for its terraced, pinnacle structure, and its biological community. Like many other seamounts, Cobb Seamount acts as a biological center of diversity, and supports a dense oceanic ecosystem. Relatively convenient access and an interesting biological setting have made the seamount an object of several scientific cruises and dives. (en) 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 , nello Stato di Washington degli Stati Uniti d'America. (it)
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dbp:age about 3.3 million (en)
dbp:discoveredBy MV John N. Cobb, 1950 (en)
dbp:mapCaption Bathymetry of the seamount (en)
dbp:name Cobb Seamount (en)
dbp:type Seamount , guyot (en)
dbp:volcanicGroup dbr:Cobb–Eickelberg_Seamount_chain
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gold:hypernym dbr:Seamount
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rdfs:comment 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 , nello Stato di Washington degli Stati Uniti d'America. (it) Cobb Seamount is a seamount (underwater volcano) 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 (FWS 1601). By 1967, over 927 km (576 mi) of soundings and dozens of samples from the seamount had been collected. (en)
rdfs:label Cobb Seamount (en) Cobb Seamount (it)
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geo:long -130.783340 (xsd:float)
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foaf:depiction wiki-commons:Special:FilePath/Monanchora_arbuscula_(Red_encrusting_sponge).jpg
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