Brule Formation | |
---|---|
Stratigraphic range: Rupelian ~ | |
Type | Geological formation |
Unit of | White River Group |
Underlies | Sharps Formation, Arikaree Formation |
Overlies | Chadron Formation |
Thickness | 6–65 metres (20–213 ft)[1] |
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 was deposited between 33 and 30 million years ago, roughly the Rupelian age (Oligocene).[2] It occurs as a subunit of the White River Group in South Dakota, Nebraska, Colorado, North Dakota, and Wyoming.
It is a sequence of fine grained clastic rocks (claystones, mudstones, siltstones) interbedded with freshwater carbonates, volcanic ash (tuff), and sandstone.[1]