Puneet Varma (Editor)

Bald Eagle Formation

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Type
  
sedimentary

Parent range
  
Thickness
  
275 +/-25 m

Named by
  
A. W. Grabau

Primary
  
Sandstone

Underlies
  

Extent
  
Pennsylvania, Maryland, West Virginia

The Ordovician Bald Eagle Formation is a mapped bedrock unit in central Pennsylvania, USA. It is a ridge-forming unit in the Appalachian Mountains.

Contents

Description

The Bald Eagle is defined as a gray to olive-gray and grayish-red, fine to coarse-grained crossbedded sandstone or greywacke. A conglomeratic member, called the Lost Run Member, exists in some locations.

Depositional environment

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

Fossils

Very few fossils exist in the Bald Eagle Formation, and most of them are trace fossils. However, at the base of the formation is the Orthorynchula biostratigraphic marker bed, which contains abundant Orthorynchula brachiopods.

Age

Relative age dating of the Bald Eagle places it in the Upper Ordovician period, being deposited between 488.3 and 443.7 (±10) million years ago. It rests conformably atop the Reedsville Formation and conformably below the Juniata Formation.

Economic Uses

The Bald Eagle is a good source of road material, riprap and building stone. However, iron pyrite inclusions may lead to acidic rainwater runoff.

References

Bald Eagle Formation Wikipedia


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