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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.

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  • Strand Fiord Formation (en)
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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. (en)
name
  • Strand Fiord Formation (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Dragon_Cliffs,_Nunavut.jpg
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  • Dragon Cliff, including the flood basalt lava layers (en)
country
  • Canada (en)
period
  • Late Cretaceous (en)
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  • 79.2311111111111 -91.86888888888889
has 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)
namedby
  • Souther, 1963 (en)
namedfor
  • Strand Fiord (en)
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  • POINT(-91.86888885498 79.231109619141)
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