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Statements

Subject Item
dbr:Patton_Seamount
rdf:type
yago:GeologicalFormation109287968 yago:Vent109470550 yago:WikicatSeamountsOfTheCobb-EickelbergSeamountChain yago:YagoLegalActorGeo yago:YagoPermanentlyLocatedEntity yago:YagoGeoEntity yago:Object100002684 geo:SpatialThing yago:Opening109379111 yago:AmorphousShape113867492 yago:Attribute100024264 yago:Space113910384 yago:Location100027167 yago:NaturalElevation109366317 yago:PhysicalEntity100001930 yago:Mountain109359803 yago:Shape100027807 yago:WikicatHotspotVolcanoes yago:Seamount109427752 yago:Abstraction100002137 yago:Crack109258715 yago:WikicatSubmarineVolcanoes
rdfs:label
Patton Seamount Patton Seamount
rdfs:comment
Il Patton Seamount è una montagna sottomarina, e più precisamente un vulcano sottomarino, che fa parte della catena sottomarina di Cobb-Eickelberg ed è situato nel Golfo dell'Alaska, nella parte nordorientale dell'Oceano Pacifico. Si trova circa 166 miglia nautiche (307 km) a est dell'Isola Kodiak e si innalza fino a 160 m al di sotto della superficie del mare; il Patton è una delle più importanti montagne della catena sottomarina di Cobb-Eickelberg. Patton Seamount is a prominent seamount (underwater volcano) in the Cobb–Eickelberg Seamount chain in the Gulf of Alaska. Located 166 nmi (307 km; 191 mi) east of Kodiak Island and reaching to within 160 m (520 ft) of the ocean surface, Patton is one of the largest seamounts in the Cobb–Eickelberg Seamount chain. It was originally created near the coast of Oregon by the Cobb hotspot 33 million years ago, and was moved to its present location by tectonic plate movement. Patton is one of the most well-understood seamounts, as a major expedition using DSV Alvin in 1999 and another in 2002 helped define the scope of the seamount's biological community. Like other large seamounts, Patton acts as an ecological hub for sea life. Dives have revealed that the volcano is heavily encrusted in sea lif
dbp:name
Patton Seamount
geo:lat
54.58000183105469
geo:long
-150.4400024414062
foaf:depiction
n9:Patton_basalt_surface.jpg n9:Patton_Seamount.jpg n9:Macroregonia_macrochiera_on_Patton_Seamount.jpg
dct:subject
dbc:Submarine_volcanoes dbc:Hotspot_volcanoes dbc:Seamounts_of_the_Cobb–Eickelberg_Seamount_chain
dbo:wikiPageID
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dbo:wikiPageRevisionID
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dbr:Brittle_star dbr:Sea_star n14:Macroregonia_macrochiera_on_Patton_Seamount.jpg dbr:Oregon dbr:Seamount dbr:Gulf_of_Alaska dbr:Hotspot_(geology) dbr:King_crab dbr:Albatrossia dbr:Suspension_feeder dbr:Endemism dbr:Sebastolobus dbr:DSV_Alvin dbr:Pacific_Plate dbr:Macroregonia_macrochira dbr:Kodiak_Island dbr:Embassichthys_bathybius dbr:Submarine_volcano dbc:Hotspot_volcanoes dbr:Psolus dbr:Sea_anemone dbr:Sebastes dbr:Antimora_microlepis dbc:Seamounts_of_the_Cobb–Eickelberg_Seamount_chain dbr:Sessility_(zoology) dbr:Cobb_hotspot dbr:Lithodes dbr:Right_whale dbr:Coryphaenoides dbr:Coral dbr:Anoplopoma_fimbria n14:Patton_basalt_surface.jpg dbr:Plate_tectonics dbr:Florometra dbr:Sponge dbr:Cobb–Eickelberg_Seamount_chain dbr:Demersal dbr:Shortraker_rockfish dbr:Oregon_State_University dbc:Submarine_volcanoes dbr:Whale_fall
owl:sameAs
n12:4t982 yago-res:Patton_Seamount wikidata:Q7148644 dbpedia-it:Patton_Seamount freebase:m.0fq1t1j
dbp:volcanicGroup
dbr:Cobb–Eickelberg_Seamount_chain
dbp:wikiPageUsesTemplate
dbt:Ship dbt:Infobox_Seamount dbt:Short_description dbt:Convert dbt:Clear dbt:Coord dbt:Reflist
dbo:thumbnail
n9:Patton_Seamount.jpg?width=300
dbp:age
1.0414008E15
dbp:mapCaption
3
dbp:mapSize
220
dbp:type
Seamount
georss:point
54.58 -150.44
dbo:abstract
Il Patton Seamount è una montagna sottomarina, e più precisamente un vulcano sottomarino, che fa parte della catena sottomarina di Cobb-Eickelberg ed è situato nel Golfo dell'Alaska, nella parte nordorientale dell'Oceano Pacifico. Si trova circa 166 miglia nautiche (307 km) a est dell'Isola Kodiak e si innalza fino a 160 m al di sotto della superficie del mare; il Patton è una delle più importanti montagne della catena sottomarina di Cobb-Eickelberg. Si formò originariamente 33 milioni di anni fa vicino alla costa dell'Oregon in seguito all'attività del punto caldo di Cobb e si spostò successivamente nell'attuale posizione in conseguenza del movimento della placca tettonica. Il Patton Seamount è uno dei seamount meglio conosciuti, dopo che due importanti spedizioni di ricerca compiute con il sommergibile DSV Alvin nel 1999 e nel 2002 hanno permesso di approfondire la conoscenza della sua comunità biologica. Come altre montagne sottomarine il Patton agisce da centro di aggregazione per una vasta fauna marina. Le immersioni hanno rivelato una ricca fauna acquatica che include stelle marine, coralli, granchi reali, pesci pietra demersali e varie altre specie. Patton Seamount is a prominent seamount (underwater volcano) in the Cobb–Eickelberg Seamount chain in the Gulf of Alaska. Located 166 nmi (307 km; 191 mi) east of Kodiak Island and reaching to within 160 m (520 ft) of the ocean surface, Patton is one of the largest seamounts in the Cobb–Eickelberg Seamount chain. It was originally created near the coast of Oregon by the Cobb hotspot 33 million years ago, and was moved to its present location by tectonic plate movement. Patton is one of the most well-understood seamounts, as a major expedition using DSV Alvin in 1999 and another in 2002 helped define the scope of the seamount's biological community. Like other large seamounts, Patton acts as an ecological hub for sea life. Dives have revealed that the volcano is heavily encrusted in sea life of various forms, including sea stars, corals, king crabs, demersal rockfish, and other species.
gold:hypernym
dbr:Seamount
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geo:geometry
POINT(-150.44000244141 54.580001831055)