Juniata Formation

Juniata Formation
Stratigraphic range: Late Ordovician
Outcrop on U.S. Route 522 at Blacklog Narrows southeast of Orbisonia, Pennsylvania.
Typesedimentary
UnderliesOswego Formation and Tuscarora Formation
OverliesBald Eagle Formation
Thickness400–1,125 ft (122–343 m)
Lithology
Primarysandstone, siltstone, shale
Location
RegionAppalachian Mountains
ExtentMaryland, Pennsylvania, Tennessee, Virginia,[1] and West Virginia
Type section
Named forJuniata River in Pennsylvania
Named byDarton and Taff[2]

The Ordovician Juniata Formation is a mapped bedrock unit in Pennsylvania, West Virginia, Virginia, Tennessee, and Maryland. It is a relative slope-former occurring between the two prominent ridge-forming sandstone units: the Tuscarora Formation and the Bald Eagle Formation in the Appalachian Mountains.

Description

Conformable contact of overlying Tuscarora Formation (white rock, left) with underlying Juniata Formation (red rock, right) at the Narrows along rt. 30 in Bedford County, Pennsylvania.
Sample from roadcut on U.S. Route 322 near State College, Pennsylvania, showing slickensides

The Juniata is defined as a grayish-red to greenish-gray, thin- to thick-bedded siltstone, shale, and very fine to medium-grained crossbedded sandstone or subgraywacke and protoquartzite with interbedded conglomerate.[3][4] The Juniata is a lateral equivalent of the Queenston Shale in western Pennsylvania.

Depositional environment

The depositional environment of the Juniata has always been interpreted as mostly terrestrial or shallow marine deposits resulting in a molasse sequence produced by the Taconic orogeny.

Fossils

Very few fossils exist in the Juniata Formation, but different types of trace fossils such as tracks and burrows can commonly be found.

Age

Relative age dating of the Juniata places it in the Upper Ordovician period, being deposited between 488.3 and 443.7 (±10) million years ago. It rests conformably atop the Bald Eagle Formation in Pennsylvania and the Martinsburg Formation in Maryland,[4] and conformably below the Tuscarora Formation.[5]

Economic use

The Juniata is a good source of road material, riprap and building stone.[6]

References

  1. ^ Paleozoic Sedimentary Successions of the Virginia Valley & Ridge and Plateau
  2. ^ Darton, N.H., and Taff, J.A., 1896, Description of the Piedmont sheet (West Virginia-Maryland): U.S. Geological Survey Geologic Atlas of the United States, Piedmont folio, no. 28, 6 p.
  3. ^ Berg, T.M., Edmunds, W.E., Geyer, A.R. and others, compilers, (1980). Geologic Map of Pennsylvania: Pennsylvania Geologic Survey, Map 1, scale 1:250,000.
  4. ^ a b "Allegheny Plateau and Valley and Ridge". Geologic Map of Maryland. Maryland Geological Survey. 1968. Retrieved 2008-01-26.
  5. ^ Berg, T.M., et al., (1983). Stratagraphic Correlation Chart of Pennsylvania: G75, Pennsylvania Geologic Survey, Harrisburg, Pennsylvania.
  6. ^ Doden, Arnold G.; Gold, David P. (2008). "Bedrock Geologic Map of The Mc Alevys Fort Quadrangle, Huntingdon, Centre, and Mifflin Counties, Pennsylvania" (PDF). Pennsylvania Geological Survey. Archived from the original (PDF) on June 9, 2011. {{cite journal}}: Cite journal requires |journal= (help)

See also

  • v
  • t
  • e
Ph
Pz
C
Moscovian
  • Betsie Shale
  • Grundy Formation
  • Hyden Formation
  • Kendrick Shale
  • Pikeville Formation
Bashkirian
  • Bee Rock Formation
  • Hensley Shale
  • Sewannee Formation
  • Warren Point Formation
  • Lee Formation
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
    • Pinesburg Station Dolomite
    Lower
    Є
    Z
    • v
    • t
    • e
    Ph
    Cz
    Pe
    Eocene
    Igneous intrusives
    Mz
    J
    Igneous 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
    Dapingian
    Lower
    Tremadocian
    Є
    Furongian
    Stage 10
    Z
    Ediacaran


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