Finlay Limestone

The Finlay Limestone is a geologic formation in western Texas, southern New Mexico, and northern Chihuahua. It preserves fossils dating back to the early Cretaceous period.[1][2]

Finlay Limestone
Stratigraphic range: early Cretaceous
Limestone mountains of Finlay Limestone in Aquiles Serdán Municipality near Chihuahua City.
TypeFormation
UnderliesDel Norte Formation
OverliesCox Sandstone
Thickness130–426 feet (40–130 m)
Lithology
PrimaryLimestone
OtherSandstone
Location
Coordinates31.36°N 105.60°W / 31.36; -105.60
RegionNew Mexico
Texas
Chihuahua
CountryUnited States
Mexico
Type section
Named forFinlay Mountains
Named byG.B Richardson
Year defined1904
Finlay Limestone (the United States)
Finlay Limestone (Texas)

Description

The formation is composed of massive gray limestone with a few thin beds of brown sandstone, with a total thickness of 130–426 feet (40–130 m).[1][2] It is exposed in the Finlay Mountains (31.36°N 105.60°W / 31.36; -105.60),[1] the Sierra de Juarez,[3] and the Cerro de Cristo Rey uplift (31.787°N 106.546°W / 31.787; -106.546).[2] The formation overlies the Cox Sandstone[1] and is overlain by the Del Norte Formation.[2]

Fossils

The formation contains fossils characteristic of early Cretaceous Albian and Comanchean age.[2]

History of investigation

The formation was first defined by G.B. Richardson in 1904 and assigned to the Fredericksburg Group.[1]

See also

Footnotes

  1. Richardson 1904
  2. Lovejoy 1976
  3. Kottlowski 1973

References

  • Kottlowski, F.E. (1973). "Pre-Pliocene rocks in La Mesa region, southern Dona Ana County, New Mexico". El Paso Geological Society Field Trip Guidebook. 7: 37–46.
  • Lovejoy, E.M.P. (1976). "Geology of Cerro de Cristo Rey uplift, Chihuahua and New Mexico" (PDF). New Mexico Bureau of Mines and Mineral Resources Memoir. 31. Retrieved 3 August 2020.
  • Richardson, G.B. (1904). "Report of a reconnaissance in Trans-Pecos Texas north of the Texas and Pacific Railway". University of Texas, Mineral Survey Bulletin. 9.
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