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The Northern Cordilleran Volcanic Province (NCVP), formerly known as the Stikine Volcanic Belt, is a geologic province defined by the occurrence of Miocene to Holocene volcanoes in the Pacific Northwest of North America. This belt of volcanoes extends roughly north-northwest from northwestern British Columbia and the Alaska Panhandle through Yukon to the Southeast Fairbanks Census Area of far eastern Alaska, in a corridor hundreds of kilometres wide. It is the most recently defined volcanic province in the Western Cordillera. It has formed due to extensional cracking of the North American continent—similar to other on-land extensional volcanic zones, including the Basin and Range Province and the East African Rift. Although taking its name from the Western Cordillera, this term is a geolog

AttributesValues
rdf:type
rdfs:label
  • Northern Cordilleran Volcanic Province (en)
  • Provincia vulcanica della Cordigliera settentrionale (it)
  • Province volcanique de la cordillère septentrionale (fr)
rdfs:comment
  • La province volcanique de la cordillère septentrionale (en anglais Northern Cordilleran Volcanic Province), anciennement « ceinture volcanique de Stikine », est une province géologique de Colombie-Britannique, du Yukon et d'Alaska. Elle chevauche la chaîne Côtière et les montagnes Intérieures. Elle comprend notamment Hoodoo Mountain, le complexe volcanique du mont Edziza, Level Mountain et les pics Heart. (fr)
  • La provincia vulcanica della Cordigliera settentrionale, in passato chiamata provincia vulcanica di Stikine, è una provincia geologica della regione del Nord-ovest Pacifico, situata nella parte occidentale dell'America del Nord, e definita dalla presenza di vulcani risalenti a epoche che vanno dal Miocene all'Olocene. (it)
  • The Northern Cordilleran Volcanic Province (NCVP), formerly known as the Stikine Volcanic Belt, is a geologic province defined by the occurrence of Miocene to Holocene volcanoes in the Pacific Northwest of North America. This belt of volcanoes extends roughly north-northwest from northwestern British Columbia and the Alaska Panhandle through Yukon to the Southeast Fairbanks Census Area of far eastern Alaska, in a corridor hundreds of kilometres wide. It is the most recently defined volcanic province in the Western Cordillera. It has formed due to extensional cracking of the North American continent—similar to other on-land extensional volcanic zones, including the Basin and Range Province and the East African Rift. Although taking its name from the Western Cordillera, this term is a geolog (en)
name
  • Northern Cordilleran Volcanic Province (en)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Mount_Edziza,_British_Columbia.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Mount_Edziza_lava_flows.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/NCVP_map.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/NCVP_outline.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Nisga'a_Memorial_Lava_Bed_Provincial_Park.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/North_side_hoodoo_mountain.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Northern_Cordilleran_Volcanic_Province_rift.jpg
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