Strand Fiord Formation
http://dbpedia.org/resource/Strand_Fiord_Formation an entity of type: WikicatCretaceousGeologicFormations
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.
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Strand Fiord Formation
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Strand Fiord Formation
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Dragon Cliff, including the flood basalt lava layers
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Canada
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Late Cretaceous
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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.
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Souther, 1963
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Strand Fiord
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2462
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