Sorber Run
| Sorber Run | |
|---|---|
Sorber Run looking downstream near its mouth
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| Basin features | |
| Main source | valley on a mountain in Lake Township, Luzerne County, Pennsylvania between 1,940 and 1,960 feet (591 and 597 m) |
| River mouth | Bowman Creek in Noxen Township, Wyoming County, Pennsylvania 1,142 ft (348 m) 41°24′34″N 76°05′37″W / 41.40958°N 76.09369°WCoordinates: 41°24′34″N 76°05′37″W / 41.40958°N 76.09369°W |
| Progression | Bowman Creek → Susquehanna River → Chesapeake Bay |
| Basin size | 2.08 sq mi (5.4 km2) |
| Physical characteristics | |
| Length | 3.1 mi (5.0 km) |
Sorber Run is a tributary of Bowman Creek in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately 3.1 miles (5.0 km) long and flows through Lake Township in Luzerne County and Noxen Township in Wyoming County. The watershed of the stream has an area of 2.08 square miles (5.4 km2). The surficial geology in the stream's vicinity consists of alluvium and Wisconsinan Till. The watershed is designated as Exceptional Value waters and a Migratory Fishery. The stream is one of two Wilderness Trout Streams in Wyoming County.
Sorber Run begins in a valley on a mountain in Lake Township, Luzerne County. It flows east-northeast for a few tenths of a mile before turning northeast for a short distance. The stream then turns north for several tenths of a mile, flowing through a valley to the west of Sorber Mountain. It then exits Lake Township, Luzerne County and enters Noxen Township, Wyoming County. In this reach, the stream turns north-northwest for some distance before turning north. After a while, it turns north-northwest, leaves its valley, and turns north, reaching its confluence with Bowman Creek.
Sorber Run joins Bowman Creek 16.25 miles (26.15 km) upstream of its mouth.
The elevation near the mouth of Sorber Run is 1,142 feet (348 m) above sea level. The elevation of the stream's source is between 1,940 and 1,960 feet (591 and 597 m) above sea level.
For most of the length of Sorber Run, the surficial geology immediately next to it consists of alluvium. However, the surficial geology of alluvium does not extend very far from the stream before being replaced by a till known as Wisconsinan Till. In the stream's upper reaches, the surficial geology consists of Wisconsinan Till.
During the Ice Age, when the receding glacier in the valley of Bowman Creek reached the mouth of Sorber Run, the lower outlets of Glacial Lake Bowman opened. Sorber Run is classified as a High-gradient Clearwater Creek.
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