Type sedimentary Region Appalachian Mountains Underlies Tonoloway Formation Parent range Appalachian Mountains | Named by P. R. Uhler, 1905 Overlies Bloomsburg Formation Primary Sandstone, Slate | |
 | ||
Other siltstone, limestone, dolostone Extent Pennsylvania, Maryland, Virginia, West Virginia Named for Wills Creek at Cumberland, Allegany County, Maryland | ||
The Silurian Wills Creek Formation is a mapped bedrock unit in Pennsylvania, Maryland, Virginia, and West Virginia.
Contents
Description
The Wills Creek is defined as a moderately well bedded greenish-gray shale containing local limestone and sandstone zones, or more specifically as an olive to yellowish-gray, thin-bedded sandstone, calcareous shale, dolostone, argillaceous limestone, and sandstone. Red shale and siltstone occur in the lower part of the formation. The formation has a thickness between 450 feet and 600 feet in Maryland and 445 to 620 feet in Pennsylvania.
The Wills Creek forms the bedrock of the valley around and to the east of Lewistown, Pennsylvania.
Fossils
The Wills Creek Limestone contain fossils from the Pridoli to the Ludlow epoch, or 422.9 to 418.1 Ma.
Dean et al. (1985) describe the Wills Creek as sparsely fossiliferous.
Conodonts have been identified in the Wills Creek in Virginia (Ozarkodina snajdri crispa Zone).
Notable Exposures
Age
Relative age dating of the Wills Creek places it in the Silurian period. It rests conformably a top the Bloomsburg Formation and below the Tonoloway Formation.
Economic Uses
The Wills Creek is a poor source of construction material and is only suitable as common fill.