White River Formation
Geologic formation in the United States
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The White River Formation is a geologic formation of the Paleogene Period, in the northern Great Plains and central Rocky Mountains, within the United States.
TypeFormation
Sub-unitsBrule Formation,
Chadron Formation[1]
Chadron Formation[1]
OverliesPierre Shale
Thickness230–300 m (750–980 ft)[2]
| White River Formation | |
|---|---|
| Stratigraphic range: Late Eocene-Early Oligocene (Chadronian-Whitneyan) ~ | |
White River Badlands in South Dakota | |
| Type | Formation |
| Sub-units | Brule Formation, Chadron Formation[1] |
| Overlies | Pierre Shale |
| Thickness | 230–300 m (750–980 ft)[2] |
| Lithology | |
| Primary | Tuffaceous claystone, conglomerate[3] |
| Location | |
| Coordinates | 43.2°N 107.1°W |
| Approximate paleocoordinates | 44.8°N 98.4°W |
| Region | Colorado, Nebraska, South Dakota, Wyoming |
| Country | United States |
| Extent | northern Great Plains and central Rocky Mountains |
| Type section | |
| Named for | White River (Missouri River tributary) |
It has been found in northeastern Colorado, Dawes County in western Nebraska, Badlands of western South Dakota, and Douglas area of southeastern Wyoming.[1]
Fossil record
The geologic formation preserves fossils dating back to the Eocene and Oligocene Epochs of the Paleogene Period, during the Cenozoic Era.[4] It contains the most complete Late Eocene−Priabonian and Early Oligocene−Rupelian vertebrate record in North America.[1][5]