Pika Formation | |
---|---|
Stratigraphic range: Middle Cambrian ~ | |
Type | Formation |
Underlies | Arctomys Formation, Deadwood Formation, or Sullivan Formation |
Overlies | Eldon Formation, Titkana Formation, or Earlie Formation |
Thickness | Up to 361 metres (1,184 ft)[1] |
Lithology | |
Primary | Calcareous mudstone |
Other | Limestone, dolomite |
Location | |
Coordinates | 51°29′40″N 116°06′05″W / 51.49444°N 116.10139°W |
Region | Canadian Rockies |
Country | Canada |
Type section | |
Named for | Pika Peak |
Named by | C.F. Deiss, 1939[2] |
The Pika Formation is a stratigraphic unit of Middle Cambrian age that is present on the western edge of the Western Canada Sedimentary Basin in the Canadian Rockies of Alberta and British Columbia.[3] It was named for Pika Peak near Lake Louise in Banff National Park by C.F. Deiss in 1939.[2] It is fossiliferous and preserves several genera of trilobites.[4] Outcrops of the Pika Formation can be seen in Banff and Jasper National Parks.[5]
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