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Newton Run

Newton Run
Newton Run looking downstream.JPG
Newton Run looking downstream from Root Hollow Lane
Basin features
Main source valley on the side of a hill in Eaton Township, Wyoming County, Pennsylvania
between 1,980 and 2,000 feet (604 and 610 m)
River mouth Roaring Run in Monroe Township, Wyoming County, Pennsylvania
856 ft (261 m)
41°27′42″N 76°01′53″W / 41.46160°N 76.03152°W / 41.46160; -76.03152Coordinates: 41°27′42″N 76°01′53″W / 41.46160°N 76.03152°W / 41.46160; -76.03152
Progression Roaring Run → Bowman CreekSusquehanna RiverChesapeake Bay
Basin size 2.55 sq mi (6.6 km2)
Physical characteristics
Length 2.7 mi (4.3 km)

Newton Run is a tributary of Roaring Run in Wyoming County, Pennsylvania, in the United States. It is approximately 2.7 miles (4.3 km) long and flows through Eaton Township and Monroe Township. The watershed of the stream has an area of 2.55 square miles (6.6 km2). The stream is not designated as an impaired waterbody. The surficial geology in its vicinity consists of alluvium, alluvial fan, Wisconsinan Till, and bedrcok.

Newton Run begins in a valley on the side of a hill in Eaton Township. It flows south-southeast for a short distance before turning south-southwest. After several tenths of a mile, the stream turns south before turning south-southwest again. After a few tenths of a mile, it turns south again and enters Monroe Township, where it turns south-southeast. A few tenths of a mile further downstream, the stream leaves its valley and turns southeast, running alongside Roaring Run for a few tenths of a mile before reaching its confluence with Roaring Run.

Newton Run joins Roaring Run 0.42 miles (0.68 km) upstream of its mouth.

Newton Run is not designated as an impaired waterbody.

The elevation near the mouth of Newton Run is 856 feet (261 m) above sea level. The elevation of the stream's source is between 1,980 and 2,000 feet (604 and 610 m) above sea level.

The surficial geology along the lower reaches of Newton Run consists of alluvium. Further away from the stream, this is flanked Wisconsinan Till and a patch of alluvial fan. In the upper reaches, the surficial geology consists of Wisconsinan Till, and the valley sides have bedrock consisting of sandstone and shale.

The watershed of Newton Run has an area of 2.55 square miles (6.6 km2). The stream is entirely within the United States Geological Survey quadrangle of Noxen.


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