Brule Formation
The Brule Formation was deposited between 33 and 30 million years ago, roughly the Rupelian age (Oligocene). It occurs as a subunit of the White River Formation in Nebraska, Colorado, North Dakota, South Dakota, and Wyoming.
Brule Formation | |
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Stratigraphic range: Rupelian ~ | |
Brule Formation in Badlands National Park | |
Type | Geological formation |
Unit of | White River Formation |
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 | Nebraska, North Dakota, South Dakota, Colorado, Wyoming |
Country | United States |
It is a sequence of fine grained clastic rocks (claystones, mudstones, siltstones) interbedded with freshwater carbonates, volcanic ash (tuff), and sandstone.
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