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Seneca Creek is a 19.6-mile-long (31.5 km) [5] tributary of the North Fork of the South Branch of the Potomac River located entirely within Pendleton County, West Virginia, USA. Seneca Creek lies within the Appalachian Mountains , in the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest .
Steer Run (West Virginia) Fifteenmile Creek (Maryland/Pennsylvania) Sideling Hill Creek (Maryland/Pennsylvania) Willett Run (West Virginia) Cacapon River (West Virginia) Sir Johns Run (West Virginia) Warm Spring Run (West Virginia) Tonoloway Creek (Maryland/Pennsylvania) Stoney Run (West Virginia) Ditch Run (West Virginia) Sleepy Creek (West ...
The North Fork South Branch below Seneca Rocks in Pendleton County, West Virginia The North Fork South Branch Potomac River , 43.6 miles (70.2 km) long, [ 4 ] forms just north of the Virginia/West Virginia border in Pendleton County at the confluence of the Laurel Fork and Straight Fork along Big Mountain 3,881 feet (1,183 m).
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Warm Spring Run is an 11.9-mile-long (19.2 km) [1] non-navigable tributary stream of the Potomac River in Morgan County of West Virginia's Eastern Panhandle. It rises on the eastern side of Warm Springs Ridge (1,115 feet) and parallels U.S. Route 522 for most of its course. Warm Spring Run enters the Potomac River at Hancock.
After it flows beneath High Street (West Virginia Route 28), Big Run parallels WV 28 moving northward and passes through the Hampshire County Industrial Park. It then flows beneath the South Branch Valley Railroad and passes the old "Cold Storage" facility and Wappocomo farm before it empties into the South Branch Potomac River .
Seneca Rocks is an unincorporated community located in Pendleton County, West Virginia, United States. [2] The community of Seneca Rocks — formerly known as Mouth of Seneca — lies at the junction of US 33, WV 28 and WV 55 near the confluence of Seneca Creek and the North Fork South Branch Potomac River.
Monongahela National Forest, West Virginia, 8 October 2017 The river begins as a series of gullies through an open marshland just south of the northernmost bend in Forest Road 112. Between river mile (RM) 12.8 and 12.4, a series of beaver dams causes the valley to transition from wetland into a string of lakes.