Brallier Formation

The Devonian Brallier Formation is a mapped bedrock unit in Pennsylvania, Maryland, West Virginia, and Virginia.

Brallier Formation
Stratigraphic range: Frasnian - Famennian[1]
Outcrop of Brallier Formation on north side of Pennsylvania Turnpike, central Bedford County, near Mile Marker 138
Type	sedimentary
Sub-units	Black Creek Siltstone Member,[2] Minnehaha Springs Member[3]
Underlies	Greenland Gap Group and Scherr Formation
Overlies	Harrell Formation
Thickness	1350 to 1800 feet in central PA[4]
Lithology
Primary	shale, sandstone
Location
Region	Appalachian Mountains
Country	United States
Extent	Maryland, Pennsylvania, Virginia, and West Virginia
Type section
Named by	Charles Butts, 1918[4]

Description

The Brallier Formation was described by Charles Butts in 1918 as a fine-grained, siliceous shale with few fine-grained sandstone layers, from outcrops in central Pennsylvania. Others expanded usage of the term to rocks in other states.

Stratigraphy

The Brallier is roughly equivalent to the Scherr Formation.

The contact with the underlying Harrell Formation is generally gradational.

Fossils

Hasson and Dennison reported the following fossils from outcrops of the lower Brallier at Keyser, West Virginia, Ridgeville, West Virginia, and McCoole, Maryland:^[5]

• Bivalvia: Buchiola retrostriata, Paracardium doris, Pterochaenia fragilis
• Cephalopoda: Bactrites, Orthoceras filosum
• Cricoconarida (class of Mollusca): Styliolina fissurella
• Annelida: Pteridichnites biseriatus

Notable Exposures

Type locality is at a railway station 6 miles northeast of Everett, Bedford County, Pennsylvania.^[4]

A large exposure is located in Huntingdon, Pennsylvania, along the ramp from U.S. Route 22 west to Route 26 north.^[6]

• 
  Part of the exposure at Huntingdon (2017)
• 
  Another view at Huntingdon (1924)

Another good exposure is on the Pennsylvania Railroad bed just west of Altoona, Pennsylvania.^[6]

Age

Relative age dating places the Brallier in the late Devonian.