The Bald Eagle is defined as a gray to olive-gray and grayish-red, fine to coarse-grained crossbeddedsandstone or greywacke. A conglomeratic member, called the Lost Run Member, exists in some locations.[3]
Depositional environment
The depositional environment of the Bald Eagle 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 Bald Eagle Formation, and most of them are trace fossils. However, at the base of the formation is the Orthorynchulabiostratigraphic marker bed, which contains abundant Orthorynchulabrachiopods.
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.[4]
The Bald Eagle is a good source of road material, riprap and building stone.[5] However, iron pyrite inclusions may lead to acidic rainwater runoff.
References
^Faill, R.T., Glover, A.D., and Way, J.H., 1989, Geology and mineral resources of the Blandburg, Tipton, Altoona, and Bellwood quadrangles, Blair, Cambria, Clearfield and Centre Counties, Pennsylvania: Pennsylvania Geological Survey Topographic and Geologic Atlas, 4th series, 86, 209 p., scale 1:24,000 and 1:48,000
^Grabau, A.W., 1909, Physical and faunal evolution of North America during Ordovicic, Siluric, and Early Devonic time: Journal of Geology, v. 17, p. 209-252.
