Misplaced Pages

Greenbrier Group

Article snapshot taken from Wikipedia with creative commons attribution-sharealike license. Give it a read and then ask your questions in the chat. We can research this topic together.
Lithostratigraphic unit
Greenbrier Limestone
Stratigraphic range: Middle Mississippian
The Sinks of Gandy (an underground stream) is developed in the Greenbrier Limestone Formation in West Virginia.
Typesedimentary
Sub-unitsDenmar Limestone, Taggard Shale, Pickaway Limestone, Union Limestone, Greenville Shale, and Alderson Limestone.
UnderliesBluefield Formation
OverliesMaccrady Formation and Price Formation
Thickness120 m
Lithology
PrimaryLimestone
Location
RegionAllegheny Mountains
CountryUnited States
ExtentKentucky, Maryland, Virginia, and West Virginia
Type section
Named forGreenbrier River

The Greenbrier Limestone, also known locally as the "Big Lime", is an extensive limestone unit deposited during the Middle Mississippian Epoch (345.3 ± 2.1 – 326.4 ± 1.6 Ma), part of the Carboniferous Period. This rock stratum is present below ground in much of West Virginia and neighboring Kentucky, and extends somewhat into adjacent western Maryland and southwestern Virginia. The name derives from the Greenbrier River in West Virginia.

Greenbrier Limestone is in some places more than 400 feet (120 metres) thick, allowing it to trap large quantities of oil and gas. Since this carbonate rock erodes quickly in the region's wet climate, outcrops are not prominent and are often quarried.

The Greenbrier Limestone is subdivided into six stratigraphic units. In ascending order, they are Denmar Limestone, Taggard Shale, Pickaway Limestone, Union Limestone, Greenville Shale, and Alderson Limestone. The limestones in this interval are predominantly skeletal grainstones or packstones. The Pickaway and especially the Union contain oolitic grainstones.

Numerous solution caves are developed within the Greenbrier Formation.

See also

References

  • Haught, O.L. (1968), Structural Contour Map on the Greenbrier Limestone in West Virginia; 35 X 38 inch map.
Chronostratigraphy of Maryland
Ph
Pz
C
M
Serpukhovian
Viséan
Tournaisian
D
Upper
Famennian
Frasnian
Middle
Givetian
Eifelian
Lower
Emsian
Pragian
Lochkovian
Chronostratigraphy of Virginia
Ph
Pz
C
Moscovian
Bashkirian
M
Serpukhovian
  • Bluefield Formation
  • Bluestone Formation
  • Cove Creek Formation
  • Fido Sandstone
  • Hinton Formation
  • Princeton Formation
  • Stony Gap Formation
  • Viséan
    Tournaisian
    D
    Upper
    Famennian
    Frasnian
    Middle
    Givetian
    Eifelian
    Lower
    Emsian
    Pragian
    Lochkovian
    S
    Pridoli
    Ludlow
    Ludfordian
    Gorstian
    Wenlock
    Homerian
    Sheinwoodian
    Llandovery
    Telychian
    Aeronian
    O
    Upper
    Middle
    Lower
    Є
    Z
    Chronostratigraphy of West Virginia
    Ph
    Cz
    Pe
    EoceneIgneous intrusives
    Mz
    JIgneous intrusives
    Pz
    P
    Cisuralian
    Asselian
    C
    Gzhelian
    Kasimovian
    Moscovian
    Bashkirian
    M
    Serpukhovian
    Viséan
    Tournaisian
    D
    Upper
    Famennian
    Frasnian
    Middle
    Givetian
    Eifelian
    Lower
    Emsian
    Pragian
    Lochkovian
    S
    Pridoli
    Ludlow
    Ludfordian
    Gorstian
    Wenlock
    Homerian
    Sheinwoodian
    Llandovery
    Telychian
    Aeronian
    O
    Upper
    Hirnantian
    Katian
    Sandbian
    Middle
    Darriwilian
  • Trenton Limestone
  • Black River Group
  • Dapingian
    Lower
    Tremadocian
  • Wells Creek Formation
  • Knox Group
    Є
    Furongian
    Stage 10
    Knox Group
    Chilhowee Group
    Antietam Formation
    Harpers Formation
    Weverton Formation
    Loudoun Formation
    Z
    Ediacaran
  • Catoctin Formation

  • Stub icon

    This article about a specific stratigraphic formation in West Virginia is a stub. You can help Misplaced Pages by expanding it.

    Categories: