Kananaskis Formation
{{Short description|Geological formation}}
{{Infobox rockunit
| name = Kananaskis Formation
| image =
| caption =
| type = Formation
| age = {{Fossil range|310|297|Late Pennsylvanian}}
| period = Pennsylvanian
| prilithology = Limestone, dolomite
| otherlithology = Chert, quartzite
| namedfor = Kananaskis Range
| namedby = A. McGugan and J.E. Rapson, 1961
| region = Alberta
| country = Canada
| coordinates = {{coord|50|48|24.1|N|115|15|47.9|W|name=Kananaskis Formation|display=inline,title}}
| unitof = Spray Lakes Group
| subunits =
| underlies = Ishbel Group
| overlies = Tunnel Mountain Formation
| thickness = up to about 55 metres (180 ft)
| extent =
| area =
| map =
| map_caption =
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The Kananaskis Formation is a geologic formation that is present on the western edge of the Western Canada Sedimentary Basin in the southern Canadian Rockies of western Alberta.{{Cite web|url=http://ags.aer.ca/reports/atlas-of-the-western-canada-sedimentary-basin.htm|title=The Geological Atlas of the Western Canada Sedimentary Basin (Mossop, G.D. and Shetsen, I., compilers), Chapter 14: Carboniferous Strata of the Western Canada Sedimentary Basin|author=Richards, B.C., Barclay, J.E., Bryan, D., Hartling, A., Henderson, C.M., and Hinds, R.C., Canadian Society of Petroleum Geologists and Alberta Geological Survey|year=1994|accessdate=2018-07-13|archive-date=2016-07-01|archive-url=https://web.archive.org/web/20160701131122/http://ags.aer.ca/reports/atlas-of-the-western-canada-sedimentary-basin.htm|url-status=dead}} Named after the Kananaskis Range near Banff,Glass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. {{ISBN|0-920230-23-7}}. it was deposited during the Late Pennsylvanian sub-period of the Carboniferous period.McGugan A. and Rapson, J.E. 1961. Stratigraphy of the Rocky Mountain Group (Permo-Carboniferous), Banff area, Alberta. Journal of the Alberta Society of Petroleum Geologists, vol. 9, no. 3, p. 73-106. Some of its strata host fossils of marine invertebrates.
Lithology
Paleontology
Fusulinids, spiriferid brachiopods, gastropods, and sponge spicules have been described from some of the beds in the Kananaskis Formation.McGugan, A. and Rapson, J.E. 1979. Pennsylvanian and Permian biostratigraphy, micropaleontology, petrography and diagenesis, Kananaskis valley, Alberta. Bulletin of Canadian Petroleum Geology, vol. 27, no. 4, p. 405-417.
Thickness, distribution, and relationship to other units
The Kananaskis Formation has a maximum thickness of about 55 metres (180 feet) at its type section on the west flank of Mount Chester in the Kananaskis Range. It is present in the southern Canadian Rockies of western Alberta from the Kananaskis area south to the Canada–United States border. It conformably to unconformably overlies the Tunnel Mountain Formation and is unconformably overlain by the Ishbel Group.
See also
{{Portal |Earth sciences|Canada|Paleontology}}