Alberta Group

Alberta Group Stratigraphic range: Albian to Campanian PreЄ Є O S D C P T J K Pg N
Type	Geological formation
Sub-units	Wapiabi Formation, Chungo Member, Cardium Formation, Blackstone Formation, Jumping Pound Member
Underlies	Belly River Formation
Overlies	Blairmore Group, Luscar Group, Crowsnest Formation
Thickness	up to 1,219 feet (370 m)^[1]
Lithology
Primary	Shale, sandstone
Other	Siltstone, siderite, limestone
Location
Region	Alberta
Country	Canada
Type section
Named for	Alberta
Named by	G.S. Hume, 1930

It takes the name from the province of Alberta, and was first described in outcrops along the Highwood River in southern Alberta by G.S. Hume in 1930.^[2]

Lithology

The Alberta Group is composed of silty shale for the most part. Two thick shale deposits (Blackstone Formation and Wapiabi Formation) are present above and below a sandstone sequence (the Cardium Formation). Sideritic concretions and thin argillaceous limestone beds are present within the shale stacks.^[1]

The Alberta Group occurs along the Canadian Rockies foothills from the United States-Canada border to the Athabasca River. In its type locality along the Highwood River in Southern Alberta, the group has a thickness of 610 feet (190 m). It reaches a maximum of 1,219 feet (370 m) north of the North Saskatchewan River.^[1]

The Alberta Group is conformably overlain by the Belly River Formation and rests unconformably on deposits of the Blairmore Group and Luscar Group in the Canadian Rockies foothills and on the volcanic Crowsnest Formation in southern Alberta's west. The group is equivalent with the Colorado Group and Lea Park Formation in southern Alberta's prairies, and with the Smoky Group in northern Alberta and north-east British Columbia.^[1]

The Alberta Group has the following sub-divisions from top to base:

Sub-unit	Age	Lithology	Max Thickness	Reference
Wapiabi Formation	Campanian	marine shale, which sideritic concretions, siltstone, sandstone and limestone *contains the Chungo Member sandstone	640 m (2,100 ft)	^[3]
Cardium Formation	Turonian to Coniacian	marine sandstone	108 m (350 ft)	^[4]
Blackstone Formation	Cenomanian to Turonian	marine shale and siltstone with minor limestone, sandstone and bentonite *contains the Jumping Pound Member sandstone	426 m (1,400 ft)	^[5]

1 2 3 4 Lexicon of Canadian Geologic Units. "Alberta Group". Retrieved 2009-03-01.
↑ Hume, G.S., 1930. The Highwood-Jumpingpound Anticline, with Notes on Turner Valley, New Black Diamond and Priddis Valley Structures, Alberta; Geological Survey of Canada, Summary Report 1929, Part B, pp. 1-24.
1 2 Lexicon of Canadian Geologic Units. "Wapiabi". Retrieved 2009-03-01.
↑ Lexicon of Canadian Geologic Units. "Cardium Sandstone". Retrieved 2009-03-01.
↑ Lexicon of Canadian Geologic Units. "Blackstone". Retrieved 2009-03-01.

Western Canadian Sedimentary Basin

Hydrocarbon history	Oil sands and heavy oil Frontier exploration and development Natural gas liquids Natural gas

Depositional regions	Southern Alberta Central Alberta Northwestern Alberta Plains South-central Canadian Rockies foothills North-east Plains North-central foothills Liard River Fort Nelson Northern Rocky Mountains Fort St. John Saskatchewan Western Manitoba

Canadian Rockies	Paskapoo FM Brazeau GRP St Mary FM Belly River FM Alberta GRP Wapiabi FM Cardium FM Blackstone FM Blairmore GRP Cadomin FM Kootenay GRP Fernie GRP Spray River GRP Whitehorse MBR Sulphur Mt MBR Ishbel FM Kananaskis FM Tunnel Mt FM Rundle GRP Etherington FM Mt Head FM Livingstone FM Banff FM Exshaw FM Wabamun FM Palliser FM Alexo FM Fairholme GRP Southesk FM Cairn FM Flume FM Skoki FM Outram FM Lynx FM Arctomys FM Pika FM Eldon FM Stephen FM Cathedral FM Mt Whyte FM Gog GRP Miette FM Canadian Shield

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