Puneet Varma (Editor)

Red River Formation

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Type
  
Geological formation

Other
  
breccia

Primary
  
Limestone

Underlies
  
Stony Mountain Formation

Overlies
  
Winnipeg Formation

Country
  
Canada  United States

Named for
  
Red River of the North

Sub-units
  
Fort Garry Member Selkirk Member Cat Head Member Dog Head Member

Thickness
  
up to 215 metres (710 ft)

Regions
  
Western Canadian Sedimentary Basin, Williston Basin

The Red River Formation is a stratigraphical unit of Upper Ordovician age in the Williston Basin.

Contents

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.

Subdivisions

The Red River Formation is composed of the following subdivisions from top to base:

  • Fort Garry Member: crystalline and micritic dolomite with an argillaceous dolomite breccia in the middle
  • Selkirk Member: fossiliferous dolomitic limestone
  • Cat Head Member: cherty dolomite, becoming calcareous to the south
  • Dog Head Member: fossiliferous dolomitic limestone
  • Distribution

    The Red River Formation reaches a maximum thickness of 215 metres (710 ft) in the center of the Williston Basin. At the along the Manitoba outcrop belt, it is 150 metres (490 ft) thick and thins out northwards.

    Relationship to other units

    The Red River Formation is slightly unconformably overlain by the Stony Mountain Formation and sharply overlays the Winnipeg Formation in Manitoba, the Deadwood Formation in western Saskatchewan and the Canadian Shield in northern Manitoba.

    The lower Red River Formation is equivalent to the Yeoman Formation, while the Fort Garry Member correlates with the Herald Formation.

    References

    Red River Formation Wikipedia