Maligne Formation
Geologic formation in Canada
From Wikipedia, the free encyclopedia
The Maligne Formation 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 consists primarily of argillaceous limestone and calcareous mudstone, and was named for the Maligne River in Jasper National Park by P.W. Taylor in 1957.[1][2]
| Maligne Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Formation |
| Unit of | Fairholme Group |
| Underlies | Perdrix Formation |
| Overlies | Flume Formation |
| Thickness | Up to about 30 m (98 feet)[1] |
| Lithology | |
| Primary | Argillaceous limestone |
| Other | Calcareous mudstone, shale |
| Location | |
| Coordinates | 53°03′00″N 118°05′00″W |
| Region | Alberta British Columbia |
| Country | Canada |
| Type section | |
| Named for | Maligne River |
| Named by | P.W. Taylor, 1957.[2] |
The formation is fossiliferous and includes remains of brachiopods, crinoids, gastropods, cephalopods, and other marine animals, as well as traces made by burrowing organisms.[1]
Lithology and thickness
Distribution and relationship to other units
The Maligne Formation is present in Canadian Rocky Mountains and foothills between the Kakwa Lakes area of northeastern British Columbia and the Cline River area of west-central Alberta, a distance of about 300 km (186 mi). It overlies the Flume Formation and is overlain by the Perdrix Formation. It grades laterally into the carbonate rocks of the upper Cairn Formation.[1][3]