The Stony Mountain Formation is a stratigraphic unit of Ashgill age in the Western Canadian Sedimentary Basin. It takes the name from the community Stony Mountain, Manitoba, and was first described in the town quarry by D.B. Dowling in 1900.
Lithology
Subdivisions The Stony Mountain Formation is divided into the following sub-units:
South (Williston Basin) Penitentiary Member: argillaceous dolomite Gunn Member: interbedded calcareous shale and fossiliferous limestone North Gunton Member: crystalline dolomite Lower Stony Mountain: argillaceous dolomite
Distribution The Stony Mountain Formation occurs throughout the Williston Basin. It reaches a maximum thickness of 45 metres (150 ft) in the sub-surface at the Canada/United States border, and thins out towards the east, north and west. In Manitoba, where it is exposed at the surface in the erosion belt, it has a thickness of 30 metres (100 ft).
Relationship to other units The Stony Mountain Formation is slightly unconformably overlain by the Stonewall Formation and sharply overlays the Red River Formation or the Herald Formation.
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