Crowfoot Formation | |
---|---|
Stratigraphic range: | |
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 |
Region | Alberta Western Canadian Sedimentary Basin |
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]