Pisgah Ridge

Pisgah Mountain
Highest point
Elevation	1,557 ft (475 m)
Prominence	1,077 ft (328 m) Topographical map Summit: 1557 to Benchmark @gap near Packerton, 480 ft.
Geography
Location	Carbon County, Pennsylvania, U.S.
Parent range	Appalachian Mountains
Topo map	USGS 40075G8, 1947&'83 Tamaqua (PA) Quadrangle

Pisgah Mountain or Pisgah Ridge (on older USGS Maps) is a long ridgeline 12.5 miles (20.1 km) Tamaqua to Jim Thorpe (river gap to river gap) oriented NNE-to-SSW whose northside valley is followed by U.S. Route 209 from river gap to river gap. The ridge is a succession of peaks exceeding 1,440 feet (438.9 m) looming 300–540 feet above the towns of Lansford, Coaldale, Summit Hill, and Tamaqua in the Panther Creek valley. Near Summit Hill was the 'Sharpe Mountain' (peak), where in 1791 Phillip Ginter is documented as having discovered Anthracite leading to the formation of the Lehigh Coal Mine Company. In 1818 the Lehigh Coal Company took over the mines and the mining camp gradually became a settlement and grew into Summit Hill.

The Pisgah Ridge forms the left bank drainage divide on the south and the streams source in the east. The peak at the east end of the ridge is named Mount Pisgah and represents a hard rock knob that towers 900 feet (270 m) above the Lehigh River towns of Jim Thorpe to the east, and Nesquehoning to its north. The municipalities are located relative to one another just around a near ninety-degree bend in the Lehigh a few miles apart by road or river.

Geologically, the Pisgah Ridge divide is classed as of semi-major degree, the waters enter the same body, the Delaware, but do so over fifty miles apart as the north draining waters are feed waters of the Panther Creek running east as a Little Schuylkill tributary, whilst the eastern south slope waters drain into the valley formed by the Mauch Chunk Ridge paralleling Pisgah Ridge to the south, via the Mauch Chunk Creek (White Bear Creek).

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Wikipedia