Park City Formation | |
---|---|
Stratigraphic range: Kungurian-Guadalupian, ~ | |
Type | Formation |
Underlies | Dinwoody Formation |
Overlies | Weber Formation, Tensleep Formation |
Area | 60,000 square kilometers |
Thickness | 300-30 meters |
Location | |
Region | Montana, Utah, Idaho, Wyoming |
Country | United States |
Type section | |
Named by | Boutwell, 1906 |
This article includes a list of general references, but it lacks sufficient corresponding inline citations. (March 2024) |
The Park City Formation is a fossiliferous sedimentary formation from the late Permian of Utah, Idaho, Wyoming, and Montana. It is defined by its cherty, gray to pinkish limestone, calcareous siltstone, and cherty sandstone. The rocks in this formation formed along a shallow marine continental shelf and were regularly interrupted by the Phosphoria Formation due to tectonic forces and sea level change.