The Slave Point Formation is a stratigraphical unit of Middle Devonian age in the Western Canadian Sedimentary Basin.

Law in 1955,[3] based on lithology encountered in the California Standard Steen River 2-22-117-5W6M well in Alberta.

The Slave Point Formation is composed of brown limestone, crystalline dolomite and shale laminae.

[1] It contains stromatoporoids in north-eastern British Columbia and southern Northwest Territories and in the Peace River Arch.

[1] It occurs in southern Northwest Territories, northeastern British Columbia and northern Alberta.