Cairn Formation | |
---|---|
Stratigraphic range: Frasnian ~ | |
Type | Formation |
Unit of | Fairholme Group |
Underlies | Southesk Formation |
Overlies | Flume Formation |
Thickness | Up to 180 m (590 ft) |
Lithology | |
Primary | Dolomite |
Other | Limestone, chert |
Location | |
Coordinates | 52°38′N 116°58′W / 52.633°N 116.967°W |
Approximate paleocoordinates | 13°30′S 44°24′W / 13.5°S 44.4°W |
Region | Alberta |
Country | Canada |
Type section | |
Named for | Cairn River, Alberta |
Named by | D.J. McLaren |
Year defined | 1955[1] |
The Cairn Formation is a geologic formation of Late Devonian (Frasnian) age in the Western Canada Sedimentary Basin.[2] It was named for the Cairn River near its junction with the Southesk River in Jasper National Park by D.J. McLaren in 1955.[1]
The Cairn Formation is stratigraphically equivalent to the Leduc Formation, which is a major oil-producing formation in central Alberta. Like the Leduc Formation, it was deposited in reef environments and is highly fossiliferous.[3][4] Extensive outcrops of the Cairn Formation near Canmore, Alberta are a popular field trip destination for those wishing to learn about Devonian reefs. They are also popular with rock climbers who enjoy the challenges presented by their extremely irregular surfaces.
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: CS1 maint: multiple names: authors list (link)