Strand Fiord Formation
Strand Fiord Formation Stratigraphic range: Late Cretaceous | |
---|---|
| |
Type | Geological formation |
Underlies | Kanguk Formation |
Overlies | Bastion Ridge Formation |
Lithology | |
Primary | Sill |
Other | Pyroclastic flow |
Location | |
Coordinates | 79°13′52″N 91°52′08″W / 79.231°N 91.869°W |
Region |
|
Country |
|
Type section | |
Named for | Strand Fiord |
Named by | Souther, 1963[1] |
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 Cliffs 300 m (984 ft) tall.
The Strand Fiord Formation contains columnar jointing units that are usually 1 m (3 ft) to 3 m (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 Amerasian Basin.[2] The Strand Fiord Formation is also part of the High Arctic Large Igneous Province.
See also
References
- ↑ Lexicon of Canadian Geological Units. Strand Fiord Formation
- ↑ Volcanic style in the Strand Fiord Formation (Upper Cretaceous), Axel Heiberg Island, Canadian Arctic Archipelago Retrieved on 2007-08-15
This article is issued from
Wikipedia.
The text is licensed under Creative Commons - Attribution - Sharealike.
Additional terms may apply for the media files.