Slave Point Formation

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Slave Point Formation
Stratigraphic range: Middle Devonian
TypeGeological formation
UnderliesBeaverhill Lake Group, Waterways Formation, Horn River Formation
OverliesFort Vermilion Formation, Watt Mountain Formation, Sulphur Point Formation, Presqu'ile Formation
Thicknessup to 120 metres (390 ft)[1]
Lithology
PrimaryLimestone, dolomite
OtherShale
Location
Coordinates61°10′55″N 115°56′04″W / 61.18183°N 115.93443°W / 61.18183; -115.93443 (Slave Point Formation)
RegionWCSB
CountryCanada
Type section
Named forSlave Point, Great Slave Lake
Named byCameron, A.E., 1918

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

It takes the name from Slave Point, a promontory on the north-west shore of the Great Slave Lake, and was first described in outcrop on the southern shore of the lake and along the Buffalo River by A.E. Cameron in 1918.[2] It was subsequently defined in the subsurface by J. 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.

Distribution

Relationship to other units

References

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