Earth:Finlay Limestone

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Finlay Limestone
Stratigraphic range: Albian
Limestone mountains of Finlay Limestone in Aquiles Serdán Municipality near Chihuahua City.
TypeFormation
Unit ofFredericksburg Group
UnderliesDel Norte Formation
OverliesCox Sandstone
Thickness130–426 feet (40–130 m)
Lithology
PrimaryLimestone
OtherSandstone
Location
Coordinates [ ⚑ ] 31°22′N 105°36′W / 31.36°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
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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]

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°22′N 105°36′W / 31.36°N 105.60°W / 31.36; -105.60),[1] the Sierra de Juarez,[3] and the Cerro de Cristo Rey uplift ( [ ⚑ ] 31°47′13″N 106°32′46″W / 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 is highly fossiliferous, containing fossils characteristic of early Cretaceous Albian and Comanchean age.[2]

Economic resources

The formation includes carbonate replacement deposits of lead, zinc, and silver in northern Mexico, along the Chihuahua CRD belt.[4]

History of investigation

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

See also

  • List of fossiliferous stratigraphic units in New Mexico
  • Paleontology in New Mexico

Footnotes

  1. 1.0 1.1 1.2 1.3 1.4 Richardson 1904
  2. 2.0 2.1 2.2 2.3 2.4 Lovejoy 1976
  3. Kottlowski 1973
  4. Robertson, Ken; Megaw, Peter (June 2009). "Cinco de Mayo: A new silver, lead, and zinc discovery in northern Mexico". The Leading Edge 28 (6): 730–735. doi:10.1190/1.3148416. 

References