Porcupine Hills Formation
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| Porcupine Hills Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Geological formation |
| Underlies | erosional surface |
| Overlies | Willow Creek Formation |
| Thickness | up to 1,200 metres (3,940 ft)[1] |
| Lithology | |
| Primary | Shale |
| Other | Sandstone, mudstone, siltstone |
| Location | |
| Coordinates | 49°47′15″N 113°52′49″W / 49.78753°N 113.88020°W |
| Region | Alberta |
| Country | Canada |
| Type section | |
| Named for | Porcupine Hills (Alberta) |
| Named by | G.M. Dawson, 1883 |
The Porcupine Hills Formation is a stratigraphic unit of middle to late Paleocene age in the Western Canada Sedimentary Basin. It takes its name from the Porcupine Hills of southwestern Alberta, and was first described in outcrop by George Mercer Dawson in 1883.[2]
The Porcupine Hills Formation is composed primarily of mudstones, siltstones and sandstones. The sediments were derived from the Canadian Cordillera during tectonic uplift and erosion in the late stages of the Laramide Orogeny, and were transported eastward by river systems and deposited in fluvial and floodplain environments.[3]
The mudstones are characterized by well-developed paleosols and caliche nodules, and the sandstones are cross-bedded and cemented with calcite. In contrast to the Paskapoo Formation, an equivalent formation farther to the north, there are no coaly beds. This has given rise to the hypothesis that during the deposition of the Porcupine Hills Formation the climate was semi-arid, while the climate farther north was more humid.[3]