Carlile Shale | |
---|---|
Stratigraphic range: Turonian ~ | |
Type | Geological formation |
Unit of | Colorado Group (lower); or Benton Formation Mancos Group (NM) |
Sub-units | Juana Lopez (CO, NM) Codell Sandstone Blue Hill Shale Fairport Chalk |
Underlies | Niobrara Formation |
Overlies | Greenhorn Limestone |
Thickness | 170–230 feet (52–70 m) |
Lithology | |
Primary | Shale, chalky to carbonaceous |
Other | Limestone Sandstone Siltstone Septarians Bentonite |
Location | |
Coordinates | 38°22′34″N 104°58′44″W / 38.376°N 104.979°W |
Region | Mid-continental |
Country | United States |
Type section | |
Named for | Carlile Spring and Carlile Station, 21 mi west of Pueblo, Colorado[1] |
Named by | Gilbert |
Year defined | 1896 |
The Carlile Shale is a Turonian age Upper/Late Cretaceous series shale geologic formation in the central-western United States, including in the Great Plains region of Colorado, Kansas, Nebraska, New Mexico, North Dakota, South Dakota, and Wyoming.[2]