dbo:abstract |
The Strand Fiord Formation is a Late Cretaceous volcanic component, located on northwestern and west-central Axel Heiberg Island, Nunavut, Canada. The formation contains flood basalts which are found on western Axel Heiberg Island at Dragon Cliff 300 m (980 ft) tall. The Strand Fiord Formation contains columnar jointing units that are usually 1 to 3 m (3 to 10 ft) in diameter. The formation is interpreted to represent the cratonward extension of the Alpha Ridge, a volcanic ridge that was active during the formation of the Amerasia Basin. The Strand Fiord Formation is also part of the High Arctic Large Igneous Province. (en) |
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dbp:caption |
Dragon Cliff, including the flood basalt lava layers (en) |
dbp:country |
Canada (en) |
dbp:name |
Strand Fiord Formation (en) |
dbp:namedby |
Souther, 1963 (en) |
dbp:namedfor |
Strand Fiord (en) |
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dbr:Pyroclastic_flow |
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dbr:Bastion_Ridge_Formation |
dbp:period |
Late Cretaceous (en) |
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dbr:Sill_(geology) |
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dbr:Nunavut |
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dbr:Kanguk_Formation |
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rdfs:comment |
The Strand Fiord Formation is a Late Cretaceous volcanic component, located on northwestern and west-central Axel Heiberg Island, Nunavut, Canada. The formation contains flood basalts which are found on western Axel Heiberg Island at Dragon Cliff 300 m (980 ft) tall. (en) |
rdfs:label |
Strand Fiord Formation (en) |
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freebase:Strand Fiord Formation yago-res:Strand Fiord Formation wikidata:Strand Fiord Formation https://global.dbpedia.org/id/4vSXr |
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wikipedia-en:Strand_Fiord_Formation?oldid=1084550397&ns=0 |
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