Sassenach Formation
Geologic formation in Alberta, Canada
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The Sassenach Formation is a stratigraphic unit of Late Devonian (early Famennian) age. It is present on the western edge of the Western Canada Sedimentary Basin in the Rocky Mountains and foothills of Alberta. It consists primarily of mudstone, siltstone, and silty carbonate rocks, and was named for Mount Sassenach in Jasper National Park by D. J. McLaren and E. W. Mountjoy in 1962.[1][2]
| Sassenach Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Formation |
| Underlies | Palliser Formation |
| Overlies | Mount Hawk Formation, Southesk Formation |
| Thickness | Up to about 245 metres (800 ft)[1] |
| Lithology | |
| Primary | Mudstone, siltstone |
| Other | Limestone, dolomite |
| Location | |
| Coordinates | 53°10′00″N 118°14′00″W |
| Region | Alberta |
| Country | Canada |
| Type section | |
| Named for | Mount Sassenach |
| Named by | D.J. McLaren and E.W. Mountjoy, 1962.[2] |
The Sassenach Formation was deposited near the beginning of the Fammenian stage of the Devonian, following the Frasnian–Fammenian extinction event.[3][4] It includes fossil conodonts.[5]
Lithology and thickness
Distribution and relationship to other units
The Sassenach Formation is present in the Rocky Mountains and foothills of Alberta, extending from northern Jasper National Park to the North Saskatchewan River, and it has also been tentatively recognized in some areas farther south. It overlies the Southesk Formation or the Mount Hawk Formation, depending on the location. It is overlain by the Palliser Formation, and is laterally equivalent to the upper beds of the Alexo Formation.[1][6]