Ravenscrag Formation
| Ravenscrag Formation Stratigraphic range: Late Cretaceous to Tertiary |
|
|---|---|
| Type | Geological formation |
| Sub-units | Upper Ravenscrag Lower Ravenscrag |
| Underlies | Swift Current Formation erosional surface |
| Overlies | Frenchman Formation Battle Formation Whitemud Formation Eastend Formation Bearpaw Formation |
| Thickness | up to 244 metres (800 ft)[1] |
| Lithology | |
| Primary | Claystone |
| Other | Sandstone, coal |
| Location | |
| Coordinates | 49°30′07″N 108°58′33″W / 49.50182°N 108.97585°WCoordinates: 49°30′07″N 108°58′33″W / 49.50182°N 108.97585°W |
| Region | WCSB |
| Country | |
| Type section | |
| Named for | Ravenscrag, Saskatchewan |
| Named by | N.B. Davis, 1918 |
The Ravenscrag Formation is a stratigraphical unit of Late Cretaceous to Tertiary age in the Western Canadian Sedimentary Basin.
It takes the name from the settlement of Ravenscrag, Saskatchewan, and was first described in outcrop at Ravenscrag Butte near Frenchman River by N.B. Davis in 1918.[2]
Lithology
The Ravenscrag Formation is composed of arenaceous claystone, with sandstone and coal interbeds. [1]
Distribution
The Ravenscrag Formation reaches a maximum thickness of 244 metres (800 ft) and is present as the erosional surface in south-western Saskatchewan and in the Cypress Hills area.[1]
Relationship to other units
The Ravenscrag Formation is conformably overlain by the Swift Current Formation where not eroded and conformably overlays the Frenchman Formation or separated by an erosional surface from the underlying Battle Formation, Whitemud Formation, Eastend Formation or Bearpaw Formation.[1]
It is equivalent to the Lance Formation in Montana, the Brazeau Formation of the foothills of Alberta and the Paskapoo Formation in southern Alberta.
