Graneros Shale

The Graneros Shale is a geologic formation in the United States identified in the Great Plains as well as New Mexico that dates to the Cenomanian Age of the Cretaceous Period. It is defined as the finely sandy argillaceous or clayey near-shore/marginal-marine shale that lies above the older, non-marine Dakota sand and mud, but below the younger, chalky open-marine shale of the Greenhorn. This definition was made in Colorado by G. K. Gilbert and has been adopted in other states that use Gilbert's division of the Benton's shales into Carlile, Greenhorn, and Graneros. These states include Kansas, Texas, Oklahoma, Nebraska, and New Mexico as well as corners of Minnesota and Iowa. North Dakota, South Dakota, Wyoming, and Montana have somewhat different usages — in particular, north and west of the Black Hills, the same rock and fossil layer is named Belle Fourche Shale.

Graneros Shale
Stratigraphic range:
Graneros Shale at outlet of El Vado Reservoir, New Mexico, USA
TypeFormation
Unit ofColorado Group (Great Plains)
Benton Group (Colorado, South Dakota)
Mancos Group (Colorado, New Mexico)
Sub-unitsSee text
UnderliesGreenhorn Formation
OverliesDakota Formation
Thickness114–1,000 feet (35–305 m)
Lithology
PrimaryShale
OtherSandstone, limestone
Location
Coordinates38.2763°N 104.7121°W / 38.2763; -104.7121
RegionColorado, Iowa, Kansas, Minnesota, Montana, New Mexico, Nebraska, North Dakota, South Dakota, Wyoming
Country United States
Type section
Named forGraneros Creek, Walsenburg quadrangle, Pueblo Colorado
Named byG.K. Gilbert (from R.C. Hills)
Year defined1896
Graneros Shale (the United States)
Graneros Shale (Colorado)
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