Brule Formation
| Brule Formation | |
|---|---|
| Stratigraphic range: Rupelian ~ | |
Brule Formation in Badlands National Park | |
| Type | Geological formation |
| Unit of | White River Group |
| Underlies | Sharps Formation, Arikaree Formation |
| Overlies | Chadron Formation |
| Thickness | 6–65 metres (20–213 ft) |
| Lithology | |
| Primary | Fine grained clastic rocks |
| Other | Freshwater limestone, tuff, sandstone |
| Location | |
| Region | South Dakota, Nebraska, North Dakota, Colorado, Wyoming |
| Country | United States |
The Brule Formation is a sequence of fine grained clastic rocks (claystones, mudstones, siltstones) interbedded with freshwater carbonates, volcanic ash (tuff), and sandstonein South Dakota, Nebraska, Colorado, North Dakota, and Wyoming. It was deposited between 34 and 30 million years ago, roughly the Rupelian age (Oligocene). It occurs as a subunit of the White River Group.