Kaskapau Formation
| Kaskapau Formation Stratigraphic range: Turonian to Coniacian |
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|---|---|
Kaskapau Shale
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| Type | Geological formation |
| Unit of | Smoky River Group |
| Sub-units | Doe Creek Member, Pouce Coupe Member, Wartenbe Member, Tuskoola Member |
| Underlies | Bad Heart Formation, Cardium Formation |
| Overlies | Dunvegan Formation |
| Thickness | up to 900 meters (3,000 ft) |
| Lithology | |
| Primary | Carbonaceous shale |
| Other | Sandstone tongues and lenticles, volcanic ash |
| Location | |
| Coordinates | 55°55′N 118°38′W / 55.917°N 118.633°WCoordinates: 55°55′N 118°38′W / 55.917°N 118.633°W |
| Region | Western Canadian Sedimentary Basin |
| Country |
 Canada
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| Type section | |
| Named by | McLearn, 1926 |
The Kaskapau Formation is a geological formation in North America whose strata date back to the Late Cretaceous.
The name derives from kaskapahtew (ᑲᐢᑲᐸᐦᑌᐤ), the Cree word for "smoky". It was first described on the banks of the Smoky River, close to the confluence with the Puskwaskau River by F.H. McLearn in 1926.
The formation is 170 meters (560 ft) thick in the Peace River and Smoky River area, and thickens up to 900 meters (3,000 ft) in the foothills of the Northern Rocky Mountains in British Columbia. It is exposed along the Peace River near Dunvegan, as well as in the Smoky River area.
The formation is part of the Smoky River Group, and is conformably overlain by the Bad Heart Formation in the western area, and unconformably by the Cardium Formation in the Pouce Coupe River area. It is conformable underlain by the Dunvegan Formation.
The Kaskapau Formation is equivalent to the Colorado Group shale in central Alberta. It is equivalent to the upper Blackstone Formation, the Cardium Formation, and the Muskiki Formation in the Canadian Rockies foothills in western Alberta.
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