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ⓘ Blairmore Group. The Blairmore Group, originally named the Blairmore Formation, is a geologic unit of Early Cretaceous age in the Western Canada Sedimentary Bas ..



                                     

ⓘ Blairmore Group

The Blairmore Group, originally named the Blairmore Formation, is a geologic unit of Early Cretaceous age in the Western Canada Sedimentary Basin that is present in southwestern Alberta and southeastern British Columbia. It is subdivided into a series of formations, most of which contain plant fossils. In some areas it contains significant reservoirs of natural gas.

                                     

1. Lithology

The Blairmore group includes the conglomerate and quartzose sandstones of the Cadomin Formation at the base, and grades to sandstone, siltstone, mudstone, and limestone in the overlying formations. The Beaver Mines and Ma Butte Formations in the upper part of the group also include minor beds of bentonite and tuff.

                                     

2. Stratigraphy

The Blairmore Group is subdivided into the following formations from top to base:

Some early workers included the Crowsnest Formation, which overlies the Ma Butte Formation, at the top of the Blairmore Group, but that practice has been abandoned.

                                     

3. Distribution and Thickness

The name Blairmore Group is applicable in the foothills and mountains of southwestern Alberta and southeastern British Columbia, from the Canada–United States border northward to the Clearwater River. The equivalent strata north of the Clearwater River, which were originally assigned to the Blairmore Group, differ in that they contain major coal deposits and they have therefore been reassigned to the Luscar Group.

The Blairmore Group has a maximum thickness of about 2.000 m 6.560 ft and thins from west to east.

                                     

4. Relationship to other units

The Blairmore Group unconformably overlies the Kootenay Group and is gradationally overlain by the Crowsnest Formation or, where the Crowsnest Formation is absent, is disconformably overlain by the Alberta Group. It is equivalent to the Luscar Group north of the Clearwater River and to the Mannville Group in the plains to the east.

                                     

5. Environment of deposition and paleontology

The Blairmore Group is an eastward-thinning wedge of clastic sediments derived from the erosion of newly uplifted mountains to the west. The sediments were transported eastward by river systems and deposited in a variety of braided stream, river channel, floodplain, and coastal plain environments along the western edge of the Western Interior Seaway. Its formations include a variety of plant fossils, trace fossils, bivalves, and mircofossils.

                                     
  • Blairmore School was an independent boarding preparatory school in Glass near Huntly, Aberdeenshire until its closure in 1993. The site is now owned and
  • HMCS Blairmore pennant J314 was a Bangor - class minesweeper that served with the Royal Canadian Navy during the Second World War. Entering service in
  • interval between the Jurassic Fernie Formation and the Lower Cretaceous Blairmore Group He subdivided it into three formations as shown below and designated
  • strata encompassed by the Luscar Group were originally included in the Blairmore Group However, the Blairmore Group strata in the mountains and foothills
  • 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
  • Exshaw Formation in southern Alberta, by the Blairmore Group in western Alberta and by the Mannville Group in eastern Alberta. It rests conformably on
  • in Mozambique. The Crowsnest Formation is the uppermost unit of the Blairmore Group Exposures along the Crowsnest Highway Highway 3 and the railroad
  • Blairmore and Manville groups formed along the edge of the ocean. These shorelines were important for coal and oil and gas formation. The Blairmore Group
  • part of the Blairmore Group It disconformably overlies the Gladstone Formation and grades into the Gates Formation of the Luscar Group north of the
  • Park Formation shale and unconformably underlain by the Blairmore Mannville or Swan River Group in Western Canada. The lower part is equivalent with the


                                     
  • it contains plant fossils. The Ma Butte Formation is a unit of the Blairmore Group It consists primarily of fine - grained sandstones interbedded with
  • age. It is the basal unit of the Bullhead Group in northeastern British Columbia and of the Blairmore Group in Alberta. The formation is a distinctive
  • the lower Blairmore Group in the Canadian Rockies foothills and to the Bullhead Group and the Spirit River Formation of the Fort St. John Group in north - western
  • the Crowsnest Pass. The Gladstone Formation is a unit of the Blairmore and Luscar Groups The lower portion of the formation consists of fine - grained
  • Leach, W.W., 1914. Blairmore map - area, Alberta Geological Survey of Canada, Summary Report 1912, p. 234. with Map 107A, Blairmore Alberta, Scale: 1
  • neighbourhood remained undeveloped until the subsequent creation of the adjacent Blairmore Suburban Centre led to the final phase of Parkridge being built out in
  • Collegiate or Bethlehem Catholic High School on Bowlt Crescent a part of Blairmore SDA community. According to MLS data, the average sale price of a home
  • Communications, retaining ownership only of CFNY in Toronto. Banff Canmore - CFHC Blairmore - CJPR Calgary - CFAC Edmonton - CJCA, CJCA - FM Grande Prairie - CFGP Lethbridge
  • format at 94.9 FM under its on - air branding as Real Country 94.9 in Blairmore Alberta. The station was owned operated by Newcap Radio until they
  • Canada. It is located in the Crowsnest River Valley and is part of the Blairmore Range of the Canadian Rockies. The headwaters of the Oldman River are


                                     
  • it was revealed that its employees had managed the Smith Williamson Blairmore Global Equity Fund since 1997. This fund was founded by David Cameron s
  • reaching Highway 40 at Coleman. It continues alongside the railway through Blairmore again crossing the Crowsnest River and bisecting the community of Frank
  • Cretaceous Blairmore Group but fieldwork at the L. minimus type locality in the early 1930s showed it to be within the Belly River Group and Loris Russell
  • London, and brought up in Peasemore, Berkshire. His father was born at Blairmore House near Huntly, Aberdeenshire, and died near Toulon in France on 8
  • Kitchener - 3, 505 m 11, 499 ft Mount Lyell - 3, 504 m 11, 496 ft Bare Range Blairmore Range Blue Range Bosche Range Brazeau Range Caribou Mountains Clark Range
  • from Halifax, Nova Scotia on 28 February with escorts New Westminster, Blairmore and Rimouski. They reached New York City on 3 March 1943. Convoy Battles
  • Cadet Corps - Didsbury Disbanded 535 Royal Canadian Army Cadet Corps - Blairmore Re - badged 2383 Royal Canadian Army Cadet Corps Now affiliated with The
  • 25 metres 80 ft in the core of an anticline at Grassy Mountain near Blairmore Alberta, and extreme thickening to 120 metres 390 ft occurred in a
  • hit a mine and after damage control efforts saved the ship, sister ship Blairmore took the vessel in tow and brought her to Le Havre. Mulgrave was towed
  • Vice - President of Blairmore Holdings, an offshore fund run by David Cameron s late father Ian Cameron. He was also President of S.L.H. Group Inc, and a Director

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