Pennsylvania, United States
Bald Eagle Mountain, once known locally as Muncy Mountain, is a stratigraphic ridge in central Pennsylvania, United States, running east of the Allegheny Front and northwest of Mount Nittany. It lies along the southeast side of Bald Eagle Creek, and south of the West Branch Susquehanna River, and is the westernmost ridge in its section of the Ridge-and-valley Appalachians. The ridge line separates the West Branch Susquehanna Valley from the Nippenose and White Deer Hole Valleys, and Bald Eagle Valley from Nittany Valley.
Bald Eagle Mountain lies in the central portion of Centre County, the southern portion of Clinton County, the southern portion of Lycoming County, and the ridge line forms part of the border between Blair County and Huntingdon County. It runs from the water gap formed with Brush Mountain by the Little Juniata River at Tyrone, to the bend in the West Branch Susquehanna River just east of Williamsport, a distance of approximately 60 miles (100 km).
The Julian and Unionville Pikes are paved roads that cross the ridge near State College, along with and U.S. Route 322 and Interstate 99 which pass through the now enlarged wind gap known as "Skytop". Most other major road crossings are through gaps, including Interstate 80 which passes through the Curtin Gap east of Milesburg, Pennsylvania. There are water gaps in the ridge formed by Spring Creek in Milesburg and Fishing Creek in Mill Hall (where U.S. Route 220 crosses).
Bald Eagle Ridge is popular with soaring birds and glider pilots ridge soaring along its slopes. This ridge is part of a chain of ridges that stretch south to Tennessee. The Ridge Soaring Gliderport lies at the foot of this ridge between Julian and Unionville.
A mature oak and hickory forest covers the Bald Eagle Mountain.
It is one of the best sites in the eastern United States for viewing the migration of the golden eagle.
Geology of Bald Eagle Mountain
Bald Eagle Mountain is in the western part of the Ridge and Valley province of the Appalachian Mountains. Brush Mountain, and neighboring Nittany Mountain and Tussey Mountain ridges, are part of the same Paleozoic anticline rock formation consisting of older Ordovicial Bald Eagle Formation Sandstone and Juniata Formation Shale, and younger Silurian Tuscarora Formation Quartzite.
During the Appalachian orogeny, these layers folded up with the underlying and overlying layers into the Nittany Arch. The arch was a Himalayan scale mountain that towered above what is now Nittany Valley, where the oldest rock layers from deep within the eroded mountain are now exposed. Younger rocks from the outer layers of the arch are exposed on the West side of the ridge in the Bald Eagle Valley, with the youngest across the valley at the foot of the Allegheny Front. These sedimentary rock layers were tipped almost vertical on the side of the ancient mountain where Bald Eagle Mountain now lies.
The Tuscarora Quartzite is more resistant to erosion than Bald Eagle Sandstone, and both are more durable than the Juniata Shale sandwiched in-between. Softer rock layers on either side of these eroded, leaving the double crested Bald Eagle Mountain ridge, with a depression between the higher western and slightly lower eastern ridge lines. On the neighboring ridges that formed the opposite slope of the ancient mountain, the same three rock layers are exposed in reverse order, with the oldest rocks near the hinge of the fold. Since the rock layers on these ridges are not vertical, the Tuscarora Formation underlies a much higher crest, and the Bald Eagle Formation creates a series of lower "terraces" broken by small ravines.
The southeast slope of the ridge is underlaid by Juniata Formation sandstone. The northwest slope of the ridge, where the rock layers are near vertical, exposes a series of rock layers, from summit to foot, or older to younger: Clinton Group sandstone and shale, Mifflintown Formation shale and limestone, Bloomsburg Formation shale, siltstone, sandstone, and mudstone, Wills Creek Formation shale, siltstone, limestone, and dolomite, Tonoloway Formation limestone, Keyser Formation limestone, Old Port Formation Shriver chert, Mandata shale, Corriganville chert, New Creek limestone and Ridgeley Member sandstone, and Onondaga Formation calcareous shale.