Nesquehoning Mountain
Nesquehoning Mountain or Nesquehoning Ridge is a 15–17-mile-long (24–27 km) coal bearing ridge dividing the waters of Lehigh Valley to the north from the Schuylkill River valley and the several near parallel ridgelines of the Ridge-and-valley Appalachians barrier range all local members of which run generally WSW-ENE in the greater overall area.
| Nesquehoning Mountain | |
|---|---|
| Nesquehoning Ridge | |
| Highest point | |
| Peak | Lat/Lng:405000N 0755457W |
| Elevation | 1,535 ft (468 m) |
| Coordinates | 40°50′0″N 75°54′57″W |
| Dimensions | |
| Length | 25 mi (40 km) east-west |
| Width | 1–2 km (0.62–1.24 mi) north-south |
| Geography | |
| Country | United States |
| State | Pennsylvania |
| Borders on | Ridge-and-Valley Appalachians and Great Appalachian Valley |
| Geology | |
| Orogeny | Appalachian Mountains |
| Age of rock | Silurian |
| Type of rock | Tuscarora Formation and Shawangunk Formation; sedimentary |
Nestled above a creek sculpted ravine across from the even less negotiable sides of Broad Mountain the flanks above Nesquehoning Creek reach a sharp bend cut by the water gap of the Lehigh River and merge with the ridge of Pisgah Ridge to the south into a common terminal mountain, Mount Pisgah within sight of the Poconos in a region once touted as "The Switzerland of America" along the eastern edge of the Southern Anthracite Region, all several ridge lines north of Blue Mountain, which in part provides the source waters for Nesquehoning Creek, a tributary of the Lehigh River in the Poconos in Northeastern Pennsylvania.