Scollard Formation | |
---|---|
Stratigraphic range: Maastrichtian-Danian ~ | |
Type | Geological formation |
Unit of | Edmonton Group |
Sub-units | Ardley coal zone |
Underlies | Paskapoo Formation |
Overlies | Battle Formation |
Thickness | Up to 300 metres (980 ft)[1] |
Lithology | |
Primary | Sandstone, siltstone, shale |
Other | Coal, bentonite |
Location | |
Coordinates | 51°56′19″N 112°55′37″W / 51.93861°N 112.92694°W |
Approximate paleocoordinates | 62°48′N 86°12′W / 62.8°N 86.2°W |
Region | Alberta |
Country | Canada |
Extent | Western Canada Sedimentary Basin |
Type section | |
Named for | Scollard Canyon at Dry Island Buffalo Jump Provincial Park |
Named by | Irish, E.J.W[2] |
Year defined | 1970 |
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.
Mossop1994
was invoked but never defined (see the help page).