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.
Stratigraphic range: Turonian
Rare exposure of the Fairport Chalk member of the Carlile Shale in southern Ellis County, Kansas
|Unit of||Colorado Group (lower); or|
|Sub-units||Juana Lopez (CO, NM)|
Blue Hill Shale
|Thickness||170–230 feet (52–70 m)|
|Primary||Shale, chalky to carbonaceous|
|Named for||Carlile Spring and Carlile Station, 21 mi west of Pueblo, Colorado|
It is composed of marine deposits of the generally retreating phase (hemi-cycle) of the Greenhorn cycle of the Western Interior Seaway, which followed the advancing phase of the same cycle that formed the underlying Graneros Shale and Greenhorn Formation. As such, the lithology progresses from open ocean chalky shale (with thin limestones) to increasing carbonaceous shale to near-shore sandstone. There is a discontinuity between the top of the Carlile and the Niobrara sequence.
Viewing and accessEdit
- Auto touring in Kansas
West from mile 195, Interstate 70 leaves the level bench on the Fencepost limestone for low, broad residual hills of Carlile Shale. These low hills are mostly the Fairport Chalk member, its thin limestone beds making it more resistant than the Blue Hill Shale member. In the distance to the northwest, the Fort Hays Limestone escarpment is visible, the slopes of which are grass-covered Blue Hill Shale.
Taking the Yocemento Avenue Exit 153 south, Yocemento lies at the base of the Fort Hays bluffs. Between Yocemento and Ellis, Old Hwy 40 passes over grass-covered slump blocks of Blue Hill Shale. The Codell Sandstone member is not present in this part of the county. 14 miles south of Ellis, on Monroe St./Ellis Ave., a broad slope of blue-gray Blue Hill Shale is exposed; the soil in this area "blew out" during the Dust Bowl; many orange-tinted septarian boulders may be seen from the road.
Upper Turonian series Plesiosaur remains are among the fossils that have been recovered from the strata of its Blue Hill Shale Member in Kansas. The Carlile in eastern South Dakota contains shark teeth, fossil wood and leaves, and ammonites.
- Volcanic mineralization of the Greenhorn cycle:
- Bentonite, sedimentary volcanic ash (named for the original Graneros/Greenhorn/Carlile classification), generally showing some weathered iron stain in the Colorado Group
- Pyrite, precipitation of volcanic sulfuric acid with oceanic iron as FeS2
- Limonite, pyrite in limestone weathered to HFeO2 (rust stain or yellow ochre)
- Selenite, CaSO4 associated with Bentonite seams and ochre
- "Geologic Unit: Carlile". National Geologic Database. Geolex — Unit Summary. United States Geological Survey. Retrieved 2017-02-03.
- USGS.gov: Mineral resources of the Niobrara and Carlile Formations
- Archives.datapages.com: Stratigraphy of the Carlile Formation and Niobrara Formation (Upper Cretaceous)
- Jstor.org: "Probable plesiosaur remains from the Blue Hill Shale (Carlile Formation)" in Kansas", Kansas Academy of Science, 2009.
-  William A. Cobban and E.A. Merewether (1983), Stratigraphy and paleontology of mid-Cretaceous rocks in Minnesota and contiguous areas. USGS Professional Paper 1253.
- Alvin R. Leonard and Delmar W. Berry (1961). Geology and Ground-water Resources of Southern Ellis County and Parts of Trego and Rush Counties, Kansas, Bulletin 149. University of Kansas Publications, State Geological Survey of Kansas. p. Geologic Formations in Relation to Ground Water.
The upper 175 feet of the Carlile is classed as the Blue Hill Shale member. Most of it is blue-gray fissile argillaceous shale that contains selenite crystals and flakes of bright yellow ochre.CS1 maint: uses authors parameter (link)
|This article about a specific stratigraphic formation in the United States is a stub. You can help Wikipedia by expanding it.|