Fort St. John Group | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Sub-units | Cruiser Formation, Goodrich Formation, Hasler Formation, Gates Formation, Moosebar Formation, Shaftesbury Formation, Peace River Formation, Spirit River Formation, Bluesky Formation, Sully Formation, Sikanni Formation, Lepine Formation, Scatter Formation, Garbutt Formation, Buckinghorse Formation |
Underlies | Dunvegan Formation |
Overlies | Bullhead Group |
Thickness | up to 2,000 metres (6,560 ft) [1] |
Lithology | |
Primary | Shale |
Other | Sandstone, siltstone and conglomerates |
Location | |
Region | Northeast British Columbia Northwest Alberta Southern Yukon Southern Northwest Territories |
Country | Canada |
Type section | |
Named for | Fort St. John |
Named by | George Mercer Dawson, 1881 |
The Fort St. John Group is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin. [2] It takes the name from the city of Fort St. John, British Columbia and was first defined by George Mercer Dawson in 1881.
The Fort St. John Group is mostly composed of dark shale deposited in a marine environment. Bentonite is present in the shale, and it is interbedded with sandstone, siltstone and conglomerates.
The Fort St. John Group occurs in the subsurface in the Peace River Country of northeastern British Columbia and north-western Alberta, in southern Yukon and southern Northwest Territories. It has a thickness of 700 metres (2,300 ft) to 2,000 metres (6,560 ft).
The Fort St. John Group is conformably overlain by the Dunvegan Formation and conformably underlain by the Bullhead Group or may rest disconformably on older units.
The Fort St. John Group is subdivided into the following formations:
Sub-unit | Age | Lithology | Max. Thickness | Reference |
---|---|---|---|---|
Cruiser Formation | Albian - Cenomanian | marine shale, argillaceous siltstone and fine grained marine sandstone | 230 m (750 ft) | [3] |
Goodrich Formation | late Albian | fine-grained, laminated sandstone, mudstone partings | 400 m (1,310 ft) | [4] |
Hasler Formation | middle to late Albian | marine shale and siltstone, minor sandstone and pebble conglomerate | 265 m (870 ft) | [5] |
Commotion Formation | early to middle Albian | sandstone, shale and conglomerate | 490 m (1,610 ft) | [6] |
Gates Formation | early Albian | massive well-sorted sandstone, carbonaceous sandstone, mudstone, siltstone, coal | 263 m (860 ft) | [7] |
Moosebar Formation | early Albian | marine shale and siltstone | 289 m (950 ft) | [8] |
Sub-unit | Age | Lithology | Max. Thickness | Reference |
---|---|---|---|---|
Shaftesbury Formation | Albian | friable shale, fish scale siltstone, bentonite, ironstone | 400 m (1,310 ft) | [9] |
Peace River Formation | middle Albian | Paddy Member - greywacke, coal Cadotte Member - coarse to fine marine sandstone Harmon Member - dark, fissile, non-calcareous shale | 60 m (200 ft) | [10] |
Spirit River Formation | middle Albian | Notikewin Member - fine to medium grained argillaceous sandstone, dark shale, ironstone Falher Member - greywacke, shale, siltstone, coal Wilrich Member - dark shale thin sandstone and siltstone stringers | 348 m (1,140 ft) | [11] |
Bluesky Formation | early Albian | brown, fine to medium grained, glauconitic, porous sandstone | 46 m (150 ft) | [12] |
Sub-unit | Age | Lithology | Max Thickness | Reference |
---|---|---|---|---|
Sully Formation | early to Late Cretaceous | marine shale and siltstone | 300 m (980 ft) | [13] |
Sikanni Formation | early Cretaceous | fine-grained, calcareous, glauconitic sandstone, argillaceous siltstone and shale | 240 m (790 ft) | [14] |
Lepine Formation* | middle to late Albian | silty mudstone, sideritic concretions | 900 m (2,950 ft) | [15] |
Scatter Formation* | early to middle Albian | Bulwell Member - glauconitic sandstone Wildhorn Member - silty mudstone Tussock Member - glauconitic sandstone, silty mudstone | 375 m (1,230 ft) | [16] |
Garbutt Formation* | early Aptian | Lower Garbutt - mudstone, siltstone, siderite, bentonite Upper Garbutt - mudstone, sideritic weathering, argillaceous siltstone, laminated sandstone | 290 m (950 ft) | [17] |
Chinkeh Formation | Barremian to early Albian | sandstone with marine shale, conglomeratic base | discontinuous | [18] |
*Buckinghorse Formation is equivalent to the sum of Lepine Formation, Scatter Formation and Garbutt Formation. It occurs north-east of the Canadian Rockies foothills in British Columbia, between the Halfway River and Muskwa River. It is composed of silty marine mudstone with fine grained marine sandstone interbeds.
The Nikanassin Formation is a stratigraphic unit of Late Jurassic (Portlandian) to Early Cretaceous (Barremian) age. It is present along the western edge of the Western Canada Sedimentary Basin in western Alberta and northeastern British Columbia. Its name was first proposed by D.B. Dowling in 1909 (Coal Fields South of Grand Trunk Pacific Railway, in the foothills of the Rocky Mountain, Alberta Page 140 paragraph 4 " to this it is proposed to give the name Nikanassin, from the Cree word meaning outer range" Also it is noted on the map by D.B. Dowling.(Geological Survey of Canada. Incorrect info follows: It was named by B.R. MacKay in 1929 for the Nikanassin Range of the front-central ranges of the Canadian Rockies. Mackay did not designate a type locality for the formation, although he described outcrops near the hamlet of Brûlé, north of the Yellowhead Highway outside of Jasper National Park.
The Bluesky Formation is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin. It takes the name from the hamlet of Bluesky, and was first described in Shell's Bluesky No. 1 well by Badgley in 1952.
Gething Formation is a stratigraphic unit of Lower Cretaceous (Aptian) age in the Western Canada Sedimentary Basin. It is present in northeastern British Columbia and western Alberta, and includes economically important coal deposits.
Bullhead Group is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin of northeastern British Columbia and western Alberta. It was first defined by F.H. McLearn in 1918 as the Bullhead Mountain Formation, but later was upgraded to group status. It consists of the Cadomin and Gething Formations, although some early workers included the Bluesky Formation and others in the group.
The Kiskatinaw Formation is a stratigraphical unit of Mississippian age in the Western Canadian Sedimentary Basin.
The Muskwa Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin.
The Fernie Formation is a stratigraphic unit of Jurassic age. It is present in the western part of the Western Canada Sedimentary Basin in western Alberta and northeastern British Columbia. It takes its name from the town of Fernie, British Columbia, and was first defined by W.W. Leach in 1914.
The Spirit River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin.
The Peace River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin.
The Smoky Group is a stratigraphical unit of Late Cretaceous age in the Western Canadian Sedimentary Basin.
The Dunvegan Formation is a stratigraphical unit of Cenomanian age in the Western Canadian Sedimentary Basin.
The Schooler Creek Group is a stratigraphic unit of Middle to Late Triassic age in the Western Canadian Sedimentary Basin. It is present in northeastern British Columbia. It was named for Schooler Creek, a left tributary of Williston Lake, and was first described in two oil wells northwest of Fort St. John, by F.H. McLearn in 1921. Exposures along Williston Lake serve as a type locality in outcrop.
The Baldonnel Formation is a stratigraphical unit of Carnian age in the Western Canadian Sedimentary Basin.
The Mannville Group is a stratigraphical unit of Cretaceous age in the Western Canadian Sedimentary Basin.
The Muskiki Formation is a stratigraphical unit of Late Cretaceous age in the Western Canadian Sedimentary Basin.
The Monach Formation is a geologic formation of Early Cretaceous (Valanginian) age in the Western Canada Sedimentary Basin that consists primarily of sandstone. It is present in the northern foothills of the Canadian Rockies and the adjacent plains in northeastern British Columbia.
The Hulcross Formation is a geologic formation in the Western Canada Sedimentary Basin in northeastern British Columbia that was deposited in marine environments during the late Albian stage of the Early Cretaceous period. At one time considered to be a member of the Commotion Formation, it was elevated to formation status by D.F. Stott in 1982. It preserves ammonites and other fossils.
The Monteith Formation is a geologic formation of Early Cretaceous (Valanginian) age in the Western Canada Sedimentary Basin that consists primarily of sandstone. It is present in the northern foothills of the Canadian Rockies and the adjacent plains in northeastern British Columbia and west-central Alberta.
The Boulder Creek Formation is a geologic formation in northeastern British Columbia. It was named for a tributary to Commotion Creek in the Pine Pass area by E.M. Spieker in 1921. At one time considered to be a member of the Commotion Formation, it was elevated to formation status by D.F. Stott in 1982.
The Kootenay Group, originally called the Kootenay Formation, is a geologic unit of latest Jurassic to earliest Cretaceous age in the Western Canada Sedimentary Basin that is present in the southern and central Canadian Rockies and foothills. It includes economically important deposits of high-rank bituminous and semi-anthracite coal, as well as plant fossils and dinosaur trackways.
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