Frontier Formation

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Frontier Formation
Stratigraphic range: Cenomanian-Coniacian
Frontier Formation in Utah (Dinosaur National Monument)
TypeGeological formation
Sub-unitsTorchlight Sandstone Member, Peay Sandstone Member
UnderliesCody Shale
OverliesMowry Shale, Thermopolis Shale
Lithology
PrimarySandstone
OtherShale
Location
RegionNorth America
CountryUnited States
Extentsee text
Type section
Named byW. C. Knight, 1902[1]
Giant concretions in the Frontier Formation, northern end of the San Rafael Swell, Emery County, Utah.

The Frontier Formation is a sedimentary geological

formation whose strata date back to the Late Cretaceous. The formation's extents are: northwest Colorado, southeast Idaho, southern Montana, northern Utah, and western Wyoming
. It occurs in many sedimentary basins and uplifted areas.

The formation is described by W.G. Pierce as thick, lenticular, grey sandstone, gray shale, carbonaceous shale, and bentonite.[2]

Dinosaur remains are among the fossils that have been recovered from the formation.[3]

Vertebrate paleofauna

Other paleofauna

See also

  • List of dinosaur-bearing rock formations

References

  1. ^ W.C. Knight, 1902, Eng. and Min. Jour., v. 73, p. 721
  2. ^ Pierce, W.G., 1997, Geologic map of the Cody 1 degree x 2 degrees quadrangle, northwestern Wyoming: U.S. Geological Survey, Miscellaneous Geologic Investigations Map I-2500, scale 1:250000.
  3. .
  4. ^ "Table 17.1," in Weishampel, et al. (2004). Page 367.
  5. Geological Society of America Abstracts with Programs
    . 53 (6) – via The Geological Society of America (GSA) Connects 2021.