Nittany Valley

Coordinates: 40°54′N 77°42′W / 40.9°N 77.7°W / 40.9; -77.7
Source: Wikipedia, the free encyclopedia.
Nittany Valley
Region
814
The Little Nittany Valley looking north from Bellefonte with Sand Ridge to the right, Bald Eagle Mountain on the left, Interstate 80 in between, and Foster Joseph Sayers Reservoir in Bald Eagle State Park at the top left

Nittany Valley is an

Fishing Creek
, along with smaller streams running through Curtain Gap and Howard Gap. The northwest side of the valley between the Bald Eagle Mountain ridge and the lower Sand Ridge is also known as the Little Nittany Valley.

The valley has a mixture of farmland, woodlots, and a number of working and abandoned quarries.

Happy Valley
".

Transportation

The

short line spur that enters the valley from Milesburg, then runs along Spring Creek to Bellefonte, splits, with a track going northeast to Pleasant Gap and another going southwest to Lemont and State College. The spur to Bellefonte follows Pennsylvania Route 144 and the line from Lemont to Pleasant Gap follows Pennsylvania Route 26. Route 26 is the primary north to south route through the valley, and the Interstate 99
extension will also run along its new alignment to I-80.

Geology of Nittany Valley

Nittany Valley is in the western part of the

Himalayan scale mountain that towered above what is now the valley. The oldest rock layers from deep within the eroded mountain are now exposed on Sand Ridge in the middle of the valley. Younger rocks from the outer layers of the arch are exposed on the west side of the Bald Eagle Mountain ridge in the Bald Eagle Valley, with the youngest across that valley at the foot of the Allegheny Front. The Nittany Valley, formed in the area where the mountain once stood, is an example of inverse topography.[2]

References

  1. ^ "Nittany Valley Region".
  2. ^ a b Kempler, Steve (2007-01-19). "Geomorphology : Chapter 2 Plate T-12 : Folded Appalachians". NASA, Goddard Earth Sciences (GES), Data and Information Services Center (DISC). Archived from the original on 2007-12-06. Retrieved 2008-03-16. Nittany Valley and Morrison Cove, eroded anticlinal valleys (coves), near the western edge of the fold belt shown here … are examples of inverse topography, which is common in this geomorphic province.

40°54′N 77°42′W / 40.9°N 77.7°W / 40.9; -77.7