Reedsville Formation

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Reedsville Formation
Stratigraphic range: Late Ordovician
File:Reedsville Formation 522.jpg
Outcrop of Reedsville Formation on south side of U.S. Route 522, Blacklog Gap, Huntingdon County, Pennsylvania.
Type sedimentary
Unit of Chickamauga Group (TN only)[1]
Underlies Bald Eagle Formation
Overlies Coburn Formation in PA, Trenton Limestone in TN and WV
Lithology
Primary shale
Other sandstone
Location
Region Appalachian Mountains
Extent Pennsylvania, Maryland, Virginia, West Virginia, eastern Tennessee
Type section
Named for Reedsville, Pennsylvania
Named by E. O. Ulrich[2]

The Ordovician Reedsville Formation is a mapped surficial bedrock unit in Pennsylvania, Maryland, Virginia, West Virginia, and Tennessee, that extends into the subsurface of Ohio. This rock is a slope-former adjacent to (and stratigraphically below) the prominent ridge-forming Bald Eagle sandstone unit in the Appalachian Mountains. It is often abbreviated Or on geologic maps.

Description

The Reedsville Formation is an olive-gray to dark-gray siltstone, shale, and fine-grained sandstone.[3] In Central Pennsylvania along the Nittany Arch, and extending into the subsurface of northern West Virginia, the base of the Reedsville formation includes the black calcareous Antes Shale formation.[4]

File:Reedsville Fm calc ss.jpg
Etched section of carbonaceous sandstone bed of Reedsville Formation from along Rt. 36 near Loysburg, Bedford Co., PA. Soft-sediment deformation evident. Contains sparse fossils (black in section image) - probably brachiopods and bryozoans.

Type section

The type locality is at Reedsville, Pennsylvania.

Age

Relative age dating of the Reedsville places it in the Upper Ordovician. It rests conformably atop the Upper Ordovician Coburn Formation at the top of the Trenton Group limestone and conformably below the Bald Eagle Formation.[5]

Isotopic dating of shale mylonite in Pennsylvania reveals a K-Ar age of 372+/-8 Ma.[6]

Economic uses

The Reedsville is quarried locally in borrow pits for road material and fill.[7]

References

  1. Harris, L.D., 1965, Geologic map of the Wheeler quadrangle, Claiborne County, Tennessee, and Lee County, Virginia: U.S. Geological Survey Geologic Quadrangle Map, GQ-435, 1 sheet, scale 1:24,000 http://ngmdb.usgs.gov/Prodesc/proddesc_903.htm
  2. Ulrich, E.O., 1911, Revision of the Paleozoic systems: Geological Society of America Bulletin, v. 22, p. 281-680.
  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.
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  6. Lapham, D.M., and Root, S.I., 1971, Summary of isotopic age determinations in Pennsylvania: Pennsylvania Geological Survey Information Circular, 4th series, no. 70, 29 p.
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See also


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