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Scollard Formation information


Scollard Formation
Stratigraphic range: Maastrichtian-Danian
~70–65 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
Scollard Formation exposed along the Red Deer River, Alberta. The Tyrannosaurus rex skeleton on display at the Royal Tyrrell Museum of Palaeontology was excavated in the center of image.
TypeGeological formation
Unit ofEdmonton Group
Sub-unitsArdley coal zone
UnderliesPaskapoo Formation
OverliesBattle Formation
ThicknessUp to 300 metres (980 ft)[1]
Lithology
PrimarySandstone, siltstone, shale
OtherCoal, bentonite
Location
Coordinates51°56′19″N 112°55′37″W / 51.93861°N 112.92694°W / 51.93861; -112.92694 (Scollard Formation)
Approximate paleocoordinates62°48′N 86°12′W / 62.8°N 86.2°W / 62.8; -86.2
RegionScollard Formation Alberta
CountryScollard Formation Canada
ExtentWestern Canada Sedimentary Basin
Type section
Named forScollard Canyon at Dry Island Buffalo Jump Provincial Park
Named byIrish, E.J.W[2]
Year defined1970
Scollard Formation is located in Canada
Scollard Formation
Scollard Formation (Canada)
Scollard Formation is located in Alberta
Scollard Formation
Scollard Formation (Alberta)

The Scollard Formation is an Upper Cretaceous to lower Palaeocene stratigraphic unit of the Western Canada Sedimentary Basin in southwestern Alberta.[1][3] Its deposition spanned the time interval from latest Cretaceous to early Paleocene, and it includes sediments that were deposited before, during, and after the Cretaceous-Paleogene (K-Pg) extinction event. It is significant for its fossil record, and it includes the economically important coal deposits of the Ardley coal zone.

  1. ^ a b Cite error: The named reference Mossop1994 was invoked but never defined (see the help page).
  2. ^ Irish, E.J.W., 1970. The Edmonton Group of south-central Alberta; Canadian Society of Petroleum Geologists (CSPG), Bulletin of Canadian Petroleum Geology, vol. 18, no. 2 (June), pp. 125-155.
  3. ^ Lexicon of Canadian Geological Units. "Scollard Formation". Archived from the original on 2013-02-21. Retrieved 2009-02-06.

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