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Ishbel Group information


Ishbel Group
Stratigraphic range: Permian
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Pg
N
Calcareous siltstone exposed along the Johnston Creek west of Banff
TypeGroup
UnderliesSpray River Group
OverliesTunnel Mountain Formation, Kananaskis Formation
ThicknessUp to about 425 m (1,394 ft)[1]
Lithology
PrimaryLimestone, dolomite, sandstone
OtherChert, siltstone
Location
RegionIshbel Group Alberta
Ishbel Group British Columbia
CountryIshbel Group Canada
ExtentWestern Canadian Sedimentary Basin
Type section
Named forMount Ishbel
Named byA. McGugan
Year defined1963

The Ishbel Group is a stratigraphic unit of Permian age in the Western Canadian Sedimentary Basin. It is present in the Canadian Rockies of Alberta and British Columbia. First defined by A. McGugan in 1963,[2] it is named for Mount Ishbel of the Sawback Range in Banff National Park, and parts of the group were first described in the vicinity of the mountain at Ranger Canyon and Johnston Canyon.[3]

  1. ^ Cite error: The named reference lexicon was invoked but never defined (see the help page).
  2. ^ McGugan, A., 1963. A Permian brachiopod and fusulinid fauna from Elk Valley, British Columbia, Canada. Journal of Paleontology, v. 37, p. 621-627.
  3. ^ 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.

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