Crowfoot Formation

From Wikipedia, the free encyclopedia
Crowfoot Formation
Stratigraphic range: Frasnian
Type Geological formation
Underlies Stettler Formation
Overlies Southesk Formation
Thickness up to 38 metres (120 ft)[1]
Lithology
Primary Anhydrite, dolomite
Other Shale
Location
Coordinates 50°44′53″N 112°35′13″W / 50.748°N 112.587°W / 50.748; -112.587 (Crowfoot Formation)Coordinates: 50°44′53″N 112°35′13″W / 50.748°N 112.587°W / 50.748; -112.587 (Crowfoot Formation)
Region WCSB
Country  Canada
Type section
Named for Crowfoot Creek
Named by H.R. Belyea and D.J. McLaren, 1957

The Crowfoot Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin.

It takes the name from Crowfoot Creek, a tributary of the Bow River and was first described in the Royalite Crowfoot No. 2 well, located near the creek by H.R. Belyea and D.J. McLaren in 1957. [2]

Lithology

The Crowfoot Formation consists of anhydrite, silty dolomite, with minor shale. [1]

Distribution

The Crowfoot Formation is typically 4 metres (10 ft) thick, but can reach up to 38 metres (120 ft).[1]

Relationship to other units

The Crowfoot Formation is overlain by the Stettler Formation and overlays the Southesk Formation.[1]

It is equivalent to the Calmar Formation and part of the Graminia Formation in central Alberta and to the Torquay Formation in Saskatchewan, Manitoba and Montana.

References

  1. 1.0 1.1 1.2 1.3 Lexicon of Canadian Geologic Units. "Crowfoot Formation". Retrieved 2010-01-01. 
  2. Belyea, H.R. and McLaren, D.J., 1957. Upper Devonian nomenclature in southern Alberta. Journal of the Alberta Society of Petroleum Geologists, v. S. p.166-182.
This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.