Palliser Formation Stratigraphic range: Famennian |
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Type section near Lake Minnewanka |
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Type | Geological formation |
Sub-units | Moro Member, Costigan Member |
Underlies | Exshaw Formation |
Overlies | Alexo Formation |
Thickness | up to 580 metres (1,900 ft)[1] |
Lithology | |
Primary | Limestone |
Other | Anhydrite, Dolomite |
Location | |
Named for | Palliser Range |
Named by | Beach, 1943 |
Region | Alberta |
Country | Canada |
The Palliser Formation is a stratigraphical unit of Famennian age in the Western Canadian Sedimentary Basin. found in the ranges of the Canadian Rockies and foothills.
It was named for the Palliser Range (in turn taking its name from John Palliser, the leader of the 1850's Palliser Expedition) by H.H. Beach in 1943.[2] The type section was defined in 1994 by Meijer and Johnston in the "Devil's Gap" section south of Mount Costigan of the Palliser Range, north of Lake Minnewanka in Banff National Park.[3]
Contents |
The Palliser Formation is composed of fossiliferous, dark limestone in the upper part and massive dolomitic limestone in the lower part. [1] Anhydrite and dolomite can occur in the foothills.
The Palliser Formation is found in the main and front ranges of the Canadian Rockies, where it reaches a thickness of 580 metres (1,900 ft), as well as the foothills, where it is up to 240 metres (790 ft) thick. [1]
The Palliser Formation is unconformably overlain by the Exshaw Formation and conformably underlain by the Alexo Formation.[1]
It is equivalent to the Wabamun Group in central Alberta, with the middle part of the Three Forks Formation in Saskatchewan and Montana and with the Tetcho Formation and Kotcho Formation in the Fort Nelson area of British Columbia.
Sub-units include, from bottom to top, the Moro Member and the Costigan Member.[4]
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