Greenhorn Limestone

Greenhorn Limestone
Stratigraphic range:
Cenomanian-Turonian,
around 94.3–89.3 Ma
The Jetmore Chalk Member of the Greenhorn Formation in Kansas.
TypeFormation
Unit ofColorado Group (lower),
Benton Formation/Group,
Mancos Shale (lower), or
Cody Shale
Sub-unitsColorado members:
Bridge Creek Limestone
Hartland Shale
Lincoln Limestone
Kansas members:
Pfeifer Shale (with Fencepost ls)
Jetmore Chalk
Hartland Shale
Lincoln Limestone
UnderliesCarlile Shale
OverliesGraneros Shale
Lithology
PrimaryShale to chalky shale
Limestone, chalk to marl
Otherbentonite
Location
Coordinates38°16′37″N 104°42′47″W / 38.277°N 104.713°W / 38.277; -104.713
Regionmid-continental
CountryUnited States
Type section
Named forGreenhorn Station, 14 mi south of Pueblo, CO, and for Greenhorn Creek[1]
Named byGrove Karl Gilbert
Year defined1896[2]
Greenhorn Limestone is located in the United States
Greenhorn Limestone
Greenhorn Limestone (the United States)
Greenhorn Limestone is located in Colorado
Greenhorn Limestone
Greenhorn Limestone (Colorado)

The Greenhorn Limestone or Greenhorn Formation is a geologic formation in the Great Plains Region of the United States, dating to the Cenomanian and Turonian ages of the Late Cretaceous period. The formation gives its name to the Greenhorn cycle of the Western Interior Seaway.

  1. ^ "Geologic Unit: Greenhorn". National Geologic Database. Geolex — Unit Summary. United States Geological Survey. Retrieved 2018-03-11.
  2. ^ Donald E. Hattin (1975). Stratigraphy and Depositional Environment of Greenhorn Limestone (Upper Cretaceous) of Kansas, Kansas Geological Survey, Bulletin 209. University of Kansas Publications, State Geological Survey of Kansas. p. History of Stratigraphic Nomenclature.