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The Williston Basin is a large intracratonic sedimentary basin in eastern Montana, western North Dakota, South Dakota, southern Saskatchewan, and south-western Manitoba that is known for its rich deposits of petroleum and potash. The basin is a geologic structural basin but not a topographic depression; it is transected by the Missouri River ...
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The Big Snowy Group is a stratigraphical unit of Chesterian age in the Williston Basin. It takes the name from Big Snowy Mountains in Montana , and was first described on the north slopes of the mountain by H.W. Smith in 1935.
The Red River Formation is a stratigraphical unit of Late Ordovician age in the Williston Basin. It takes the name from the Red River of the North, and was first described in outcrop in the Tyndall Stone quarries and along the Red River Valley by A.F. Foerste in 1929. [2] [3]
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The Deadwood Formation is a geologic formation of the Williston Basin and Western Canada Sedimentary Basin.It is present in parts of North and South Dakota and Montana in the United States, and in parts of Alberta, Saskatchewan, and southwestern corner of Manitoba in Canada.
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