Spray Lakes Group | |
---|---|
Stratigraphic range: | |
Type | Group |
Sub-units | Kananaskis Formation Tunnel Mountain Formation |
Underlies | Ishbel Group |
Overlies | Rundle Group |
Thickness | More than 600 metres (2000 ft)[1] |
Lithology | |
Primary | dolomite, limestone |
Other | Sandstone, quartzite, chert |
Location | |
Coordinates | 50°48′24.1″N 115°15′47.9″W / 50.806694°N 115.263306°W |
Region | Alberta |
Country | Canada |
Type section | |
Named for | Spray Lakes, Alberta |
Named by | A. McGugan and J.E. Rapson, 1963[2] |
The Spray Lakes Group is a stratigraphic unit that is present on the western edge of the Western Canada Sedimentary Basin in the southern Canadian Rockies, and it comprises the Pennsylvanian-age strata of that region.[3] It was named after the Spray Lakes near Banff, Alberta,[1] and fossils of marine invertebrates are found in some of its strata.[4]
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: CS1 maint: multiple names: authors list (link)