About: Tasmantid Seamount Chain

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The Tasmantid Seamount Chain is a 2,000 km (1,200 mi) long chain of seamounts in the South Pacific Ocean. The chain consists of over 16 extinct volcanic peaks, many rising more than 4,000 m (13,000 ft) from the seabed. It is one of the two parallel seamount chains alongside the East Coast of Australia; the Lord Howe and Tasmantid seamount chains both run north-south through parts of the Coral Sea and Tasman Sea. These chains have longitudes of approximately 159°E and 156°E respectively.

Attributes	Values
rdf:type	Thing geo:SpatialThing
rdfs:label	Catena sottomarina della Tasmania (it) Tasmantid Seamount Chain (en)
rdfs:comment	The Tasmantid Seamount Chain is a 2,000 km (1,200 mi) long chain of seamounts in the South Pacific Ocean. The chain consists of over 16 extinct volcanic peaks, many rising more than 4,000 m (13,000 ft) from the seabed. It is one of the two parallel seamount chains alongside the East Coast of Australia; the Lord Howe and Tasmantid seamount chains both run north-south through parts of the Coral Sea and Tasman Sea. These chains have longitudes of approximately 159°E and 156°E respectively. (en) La catena sottomarina della Tasmania è una catena di montagne sottomarine lunga 2.000 km e situata nell'Oceano Pacifico meridionale. La catena consiste di oltre 16 picchi di vulcani estinti, molti dei quali si innalzano di oltre 4.000 m rispetto al fondale oceanico. È una delle due catene parallele di montagne sottomarine poste lungo la costa orientale dell'Australia; sia la catena sottomarina di Lord Howe che la catena della Tasmania si sviluppano in senso nord-sud attraverso il Mar dei Coralli e il Mar di Tasman. Le due catene hanno longitudine rispettivamente 159°E e 156°E. (it)
name	Tasmantid Seamount Chain (en)
geo:lat	-31.000000 (xsd:float)
geo:long	156.000000 (xsd:float)
foaf:depiction
dcterms:subject	Landforms of the Coral Sea Seamounts of the Pacific Ocean Miocene volcanoes Seamounts of the Tasman Sea Volcanoes of the Tasman Sea Volcanoes of Australia Guyots Tasman Sea Seamount chains Hotspot tracks
Wikipage page ID	53254105 (xsd:integer)
Wikipage revision ID	1109548614 (xsd:integer)
Link from a Wikipage to another Wikipage	Queensland Guyot Derwent Hunter Guyot Indo-Australian Plate 156th meridian east 159th meridian east Coral Sea Landforms of the Coral Sea Seabed Seamount chain Gascoyne Seamount Seamounts of the Pacific Ocean Longitude Lord Howe Seamount Chain Australia Britannia Guyots Cato Reef Miocene volcanoes Seamounts of the Tasman Sea Volcanoes of the Tasman Sea Kenn Reef Extinct volcano Tasman Sea Tasmanian Seamounts Tasmantid hotspot Taupo Bank Volcanoes of Australia Guyots Tasman Sea Seamount chains Zealandia Hotspot tracks Wreck Reefs South Pacific Ocean Seamounts East Coast of Australia dbr:Barcoo_Bank dbr:Brisbane_Guyot dbr:Fraser_Seamount dbr:Moreton_Seamount dbr:Recorder_Guyot dbr:Stradbroke_Seamount
sameAs	Tasmantid Seamount Chain Tasmantid Seamount Chain Tasmantid Seamount Chain Tasmantid Seamount Chain
dbp:wikiPageUsesTemplate	dbt:Infobox_seamount dbt:Convert dbt:Coord dbt:Distinguish dbt:Reflist dbt:Short_description
thumbnail	wiki-commons:Special:FilePath/Zealandia,_topographic_map.jpg?width=300
image caption	Topographic map of Zealandia that includes the unlabelled Tasmantid Seamount Chain off the east of Australia extending from the Coral Sea southwards into the Tasman Sea. (en)
location	Coral and Tasman seas (en)
map caption	Tasmantid Seamount Chain (en)
map size	250 (xsd:integer)
type	Seamount chain
georss:point	-31.0 156.0
has abstract	The Tasmantid Seamount Chain is a 2,000 km (1,200 mi) long chain of seamounts in the South Pacific Ocean. The chain consists of over 16 extinct volcanic peaks, many rising more than 4,000 m (13,000 ft) from the seabed. It is one of the two parallel seamount chains alongside the East Coast of Australia; the Lord Howe and Tasmantid seamount chains both run north-south through parts of the Coral Sea and Tasman Sea. These chains have longitudes of approximately 159°E and 156°E respectively. Like its neighbour, the Tasmantid Seamount Chain has resulted from the Indo-Australian Plate moving northward over a stationary hotspot. It ranges in age from 40 to 6 million years old. Alternative names for the Tasmantid Seamount Chain include the Tasmantid Seamounts, Tasman Seamounts, Tasman Seamount Chain, Tasmantide Volcanoes or simply the Tasmantids. (en) La catena sottomarina della Tasmania è una catena di montagne sottomarine lunga 2.000 km e situata nell'Oceano Pacifico meridionale. La catena consiste di oltre 16 picchi di vulcani estinti, molti dei quali si innalzano di oltre 4.000 m rispetto al fondale oceanico. È una delle due catene parallele di montagne sottomarine poste lungo la costa orientale dell'Australia; sia la catena sottomarina di Lord Howe che la catena della Tasmania si sviluppano in senso nord-sud attraverso il Mar dei Coralli e il Mar di Tasman. Le due catene hanno longitudine rispettivamente 159°E e 156°E. Coma la sua vicina, la catena sottomarina della Tasmania è stata generata dalla placca indo-australiana in movimento verso nord sopra il punto caldo della Tasmania. L'età delle montagne sottomarine che ne fanno parte è compresa tra 40 e 6 milioni di anni. (it)
prov:wasDerivedFrom	wikipedia-en:Tasmantid_Seamount_Chain?oldid=1109548614&ns=0
page length (characters) of wiki page	9077 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Tasmantid_Seamount_Chain
geo:geometry	POINT(156 -31)
is Link from a Wikipage to another Wikipage of	Queensland Guyot Derwent Hunter Guyot Coral Sea Marine Park Geology of the Pacific Ocean Louisiade Plateau Gascoyne Seamount Lord Howe Seamount Chain Hotspot (geology) Britannia Guyots Cato Reef Central Eastern Marine Park Kenn Reef Tasmanian Seamounts Tasmantid hotspot

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