Cody Shale | |
---|---|
Stratigraphic range: Late Cretaceous | |
Type | Sedimentary |
Sub-units | see text |
Underlies | Mesaverde Formation |
Overlies | Frontier Formation |
Thickness | 500-1000 m |
Lithology | |
Primary | shale |
Location | |
Region | Montana folded belt province, Central Montana uplift, Big Horn basin, Powder River basin, Wind River basin |
Country | United States |
Extent | Wyoming, Idaho, Montana |
Type section | |
Named for | Cody, Wyoming |
Named by | C. T. Lupton, 1916[1] |
The Cody Shale is a Late Cretaceous geologic formation. It is mapped in Wyoming, Idaho, and Montana.
The formation is described by W.G. Pierce as follows: upper part is buff, sandy shale and thinly laminated buff sandstone; lower part is dark gray, thin-bedded marine shale.[2]
The formation is divided into many members that vary regionally. Alphabetically:[3]
Certain members rise to formation rank in other areas; for example, the Greenhorn is classified as a formation in a number of states, particularly in Colorado and Kansas.