Spirit River Formation
Stratigraphic range: middle Albian PreꞒ Ꞓ O S D C P T J K Pg N
Falher graywake and shale
Type	Geological formation
Unit of	Fort St. John Group
Sub-units	Notikewin Member, Falher Member, Wilrich Member
Underlies	Peace River Formation
Overlies	Bluesky Formation
Thickness	up to 348 feet (110 m)[1]
Lithology
Primary	sandstone, shale, siltstone
Other	coal, ironstone, greywacke
Location
Coordinates	55°46′30″N 118°54′22″W / 55.775°N 118.906°W / 55.775; -118.906 (Imperial Spirit River No. 1 well, in 12-20-78-6W6M)
Region	Alberta, British Columbia
Country	Canada
Type section
Named for	Spirit River
Named by	Badgley, 1952

The Spirit River Formation is a stratigraphic unit of middle Albian age in the Western Canadian Sedimentary Basin.

It takes the name from the Spirit River, and was first described in Imperial Oil Spirit River No. 1 well by Badgley in 1952.^[2]

Lithology

The Spirit River Formation consists, from bottom to top of fine to medium grained argillaceous sandstone, dark shale, ironstone, greywacke, shale, siltstone, coal and dark shale with thin sandstone and siltstone stringers.^[1]

Hydraulic fracturing in Canada

'Massive' hydraulic fracturing has been widely used in Alberta since the late 1970s to recover gas from low-permeability sandstones of the Spirit River Formation.^[3]: 1044 Massive hydraulic fracturing has been widely used in Alberta since the late 1970s. The method is currently used in development of the Cardium, Duvernay, Montney and Viking formations in Alberta, Bakken formation in Saskatchewan, Montney and Horn River formations in British Columbia.

Distribution

The Spirit River Formation reaches a maximum thickness of 348 metres (1,140 ft). It is found in the sub-surface in the Peace River Country, in an area stretching from Fort St. John, British Columbia to the Lesser Slave Lake from west to east, and from Grande Prairie, Alberta to Manning, Alberta from south to north.

Relationship to other units

The Spirit River Formation is conformably overlain by the Peace River Formation and conformably underlain by the Bluesky Formation. It grades laterally to the Buckinghorse Formation shales to the north-east, and into the sandy facies of the Malcolm Creek Formation south of the Wapiti River. It is equivalent to the upper Mannville Formation in Central Alberta and to the Clearwater Formation and Grand Rapids Formation in the upper Athabasca River area.^[1]

References