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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: 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
Coordinates31°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
Finlay Limestone (the United States)
Finlay Limestone (Texas)

Description edit

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 edit

The formation is highly fossiliferous, containing fossils characteristic of early Cretaceous Albian and Comanchean age.[2]

Economic resources edit

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

History of investigation edit

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

See also edit

Footnotes edit

  1. ^ a b c d e Richardson 1904
  2. ^ a b c d e 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 edit

  • 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.

finlay, limestone, geologic, formation, western, texas, southern, mexico, northern, chihuahua, preserves, fossils, dating, back, early, cretaceous, period, stratigraphic, range, albian, preꞒ, nlimestone, mountains, aquiles, serdán, municipality, near, chihuahu. 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 LimestoneStratigraphic range Albian PreꞒ Ꞓ O S D C P T J K Pg NLimestone mountains of Finlay Limestone in Aquiles Serdan Municipality near Chihuahua City TypeFormationUnit ofFredericksburg GroupUnderliesDel Norte FormationOverliesCox SandstoneThickness130 426 feet 40 130 m LithologyPrimaryLimestoneOtherSandstoneLocationCoordinates31 22 N 105 36 W 31 36 N 105 60 W 31 36 105 60RegionNew MexicoTexasChihuahuaCountryUnited StatesMexicoType sectionNamed forFinlay MountainsNamed byG B RichardsonYear defined1904Finlay Limestone the United States Show map of the United StatesFinlay Limestone Texas Show map of Texas Contents 1 Description 2 Fossils 3 Economic resources 4 History of investigation 5 See also 6 Footnotes 7 ReferencesDescription editThe 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 editThe formation is highly fossiliferous containing fossils characteristic of early Cretaceous Albian and Comanchean age 2 Economic resources editThe formation includes carbonate replacement deposits of lead zinc and silver in northern Mexico along the Chihuahua CRD belt 4 History of investigation editThe formation was first defined by G B Richardson in 1904 and assigned to the Fredericksburg Group 1 See also edit nbsp Earth sciences portal nbsp Paleontology portalList of fossiliferous stratigraphic units in New Mexico Paleontology in New MexicoFootnotes edit a b c d e Richardson 1904 a b c d e Lovejoy 1976 Kottlowski 1973 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 editKottlowski 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 Retrieved from https en wikipedia org w index php title Finlay Limestone amp oldid 1207210644, wikipedia, wiki, book, books, library,

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