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Fairholme Group

Coordinates: 51°05′00″N 115°07′00″W / 51.08333°N 115.11667°W / 51.08333; -115.11667 (Fairholme Group)
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Fairholme Group
Stratigraphic range: Frasnian
TypeGroup
Sub-unitsMount Hawk Formation
Southesk Formation
Perdrix Formation
Cairn Formation
Maligne Formation
Flume Formation
Borsato Formation
Hollebeke Formation
UnderliesSassenach Formation, Alexo Formation, Crowfoot Formation, or Palliser Formation
OverliesBeaverhill Lake Group, Yahatinda Formation, or pre-Devonian Formations
ThicknessUp to about 730 m (2400 feet)[1]
Lithology
PrimaryLimestone, dolomite
OtherMudstone, siltstone
Location
Coordinates51°05′00″N 115°07′00″W / 51.08333°N 115.11667°W / 51.08333; -115.11667 (Fairholme Group)
Region Alberta
 British Columbia
Country Canada
Type section
Named forFairholme Range
Named byH.H. Beach[2]
Year defined1943

The Fairholme Group is a stratigraphic unit of Late Devonian (Frasnian) age. It is present on the western edge of the Western Canada Sedimentary Basin in the Rocky Mountains and foothills of Alberta and British Columbia. It was named for the Fairholme Range near Exshaw in the Canadian Rockies by H.H. Beach in 1943.[1][2]

The formations of the Fairholme Group include fossils of marine animals such as stromatoporoids, corals, brachiopods, crinoids, and conodonts.

Lithology

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The Fairholme Group was deposited in marine environments and can be subdivided into three gross lithologic units:[1]

Distribution and thickness

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The Fairholme Group is present in the Canadian Rockies from the Kakwa Lakes area of northeastern British Columbia, south through Alberta to the Flathead River region of southeastern British Columbia, as well as in the subsurface beneath the immediately adjacent plains to the east. Where fully developed, the group reaches thicknesses from about 300 to 728 m (980 to 2400 feet).[1]

Relationship to other units

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The Fairholm Group overlies the Beaverhill Lake Group in the southern Alberta plains, and unconformably overlies the Middle Devonian Yahatinda Formation or pre-Devonian formations in the mountains. It is overlain by the Crowfoot Formation in the plains, and the Sassenach, Alexo or, rarely, the Palliser Formation in the mountains. It is equivalent to the Woodbend Group and the lower part of the Winterburn Group of the plains.[1][3]

References

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  1. ^ a b c d e f g h Glass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba, p. 433-444. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. ISBN 0-920230-23-7.
  2. ^ a b Beach, H.H. 1943. Moose Mountain and Morley map-areas, Alberta. Geological Survey of Canada, Memoir 236.
  3. ^ Alberta Geological Survey. "Alberta Table of Formations, May 2019" (PDF). Alberta Energy Regulator. Retrieved 24 March 2020.

See also

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