Nazko Cone

http://dbpedia.org/resource/Nazko_Cone an entity of type: Thing

Le cône Nazko, en anglais : Nazko Cone, est un cône volcanique de Colombie-Britannique, au Canada. Il fait partie de la ceinture volcanique d'Anahim et culmine à 1 230 mètres d'altitude. rdf:langString
Il Cono Nazko è un piccolo e potenzialmente attivo cono di scorie basaltiche situato nella parte centrale della Columbia Britannica, nel Canada, circa 75 km a ovest della cittadina di Quesnel e 150 km a sudovest della città di Prince George. rdf:langString
Nazko Cone /ˈnæzkoʊ/ is a small potentially active basaltic cinder cone in central British Columbia, Canada, located 75 km west of Quesnel and 150 kilometers southwest of Prince George. It is considered the easternmost volcano in the Anahim Volcanic Belt. The small tree-covered cone rises 120 m above the Chilcotin-Nechako Plateau and rests on glacial till. It was formed in three episodes of activity, the first of which took place during the Pleistocene interglacial stage about 340,000 years ago. The second stage produced a large hyaloclastite scoria mound erupted beneath the Cordilleran Ice Sheet during the Pleistocene. Its last eruption produced two small lava flows that traveled 1 km to the west, along with a blanket of volcanic ash that extends several km to the north and east of the co rdf:langString
rdf:langString Cône Nazko
rdf:langString Cono Nazko
rdf:langString Nazko Cone
rdf:langString Nazko Cone
rdf:langString Nazko Cone
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rdf:langString below
rdf:langString Location within British Columbia
rdf:langString Nazko Cone, British Columbia.jpg
rdf:langString Nazko Cone, the easternmost and youngest volcano overlying the Anahim hotspot
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rdf:langString Nazko Cone /ˈnæzkoʊ/ is a small potentially active basaltic cinder cone in central British Columbia, Canada, located 75 km west of Quesnel and 150 kilometers southwest of Prince George. It is considered the easternmost volcano in the Anahim Volcanic Belt. The small tree-covered cone rises 120 m above the Chilcotin-Nechako Plateau and rests on glacial till. It was formed in three episodes of activity, the first of which took place during the Pleistocene interglacial stage about 340,000 years ago. The second stage produced a large hyaloclastite scoria mound erupted beneath the Cordilleran Ice Sheet during the Pleistocene. Its last eruption produced two small lava flows that traveled 1 km to the west, along with a blanket of volcanic ash that extends several km to the north and east of the cone.
rdf:langString Le cône Nazko, en anglais : Nazko Cone, est un cône volcanique de Colombie-Britannique, au Canada. Il fait partie de la ceinture volcanique d'Anahim et culmine à 1 230 mètres d'altitude.
rdf:langString Il Cono Nazko è un piccolo e potenzialmente attivo cono di scorie basaltiche situato nella parte centrale della Columbia Britannica, nel Canada, circa 75 km a ovest della cittadina di Quesnel e 150 km a sudovest della città di Prince George.
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