North Branch Potomac River Tributary to Potomac River | |
---|---|
Location | |
Country | United States |
State | West Virginia, Maryland |
County | Allegany (MD), Garrett (MD), Hampshire (WV), Mineral (WV), Grant (WV), Preston (WV) |
Cities (WV) | Bayard, Gormania, Piedmont, Keyser, Cumberland |
Cities (MD) | Kitzmiller, Luke, Westernport |
Physical characteristics | |
Source | Blackwater River divide |
• location | about 1 mile northwest of Fairfax, West Virginia |
• coordinates | 39°11′42.39″N079°29′21.19″W / 39.1951083°N 79.4892194°W [1] |
• elevation | 2,960 ft (900 m) [1] |
Mouth | Potomac River |
• location | about 1 mile east of Green Spring, West Virginia |
• coordinates | 39°31′42.33″N078°35′15.05″W / 39.5284250°N 78.5875139°W [1] |
• elevation | 525 ft (160 m) [1] |
Length | 101.27 mi (162.98 km) [2] |
Basin size | 1,343.04 square miles (3,478.5 km2) [3] |
Discharge | |
• location | Potomac River |
• average | 5.13 cu ft/s (0.145 m3/s) at mouth with Potomac River [3] |
Basin features | |
Progression | Potomac River → Chesapeake Bay → Atlantic Ocean |
River system | Potomac River |
Tributaries | |
• left | Laurel Run, Sand Run, Nyedegger Run, Glade Run, Steyer Run, Laurel Run, Crooked Run, Lostland Run, Short Run, Three Forks Run, Stony Hollow, Elklick Run, Folly Run, Laurel Run, Savage River, Georges Creek, Stony Run, Wildcat Hollow, Culvert Hollow, Dry Run, Deep Hollow, Warrior Run, Wills Creek, Collier Run, Mill Run, Seven Springs Run |
• right | Red Oak Creek, Buffalo Creek, Difficult Creek, Stony River, Maple Run, Abram Creek, Deep Run, Howell Run, Piney Swamp Run, Montgomery Run, Slaughterhouse Run, Powder House Run, Thunderhill Run, New Creek, Willow Run, Ashcabin Run, Koulip Hollow, Buckwheat Hollow, Patterson Creek, Dans Run, Round Bottom Hollow, Kern Hollow, Green Spring Run |
Waterbodies | Bloomington Lake |
Bridges | West Kempton Road (x2), Corona Bayard Road, Kitzmiller Road, Masteller Road, WV 46, US 220, Black Oak Road, WV 956, WV 28 Alt, Canal Parkway, Green Spring Road |
The North Branch Potomac River flows from Fairfax Stone in West Virginia to its confluence with the South Branch Potomac River near Green Spring, West Virginia, where it turns into the Potomac River proper.
From the Fairfax Stone, the North Branch Potomac River flows 27 miles (43 km) to the man-made Jennings Randolph Lake, an impoundment designed for flood control and emergency water supply. Below the dam, the North Branch cuts a serpentine path through the eastern Allegheny Mountains. First, it flows northeast by the communities of Bloomington, Luke, and Westernport in Maryland and then on by Keyser, West Virginia to Cumberland, Maryland. At Cumberland, the river turns southeast. 103 miles (166 km) downstream from its source, the North Branch is joined by the South Branch between Green Spring and South Branch Depot, West Virginia from whence it flows past Hancock, Maryland and turns southeast once more on its way toward Washington, D.C., and the Chesapeake Bay.
Historically, the North Branch had highly acidic water due to waste from coal mining and paper production in the region. [4] In 1969, one measuring station recorded a pH of 2.3, comparable to lemon juice. [5] : 3 This regularly killed wildlife across a 60–80 km (40–50 mi) span. It was somewhat mitigated by the construction of the Bloomington Dam, which allowed for flow control based on density. [4] The dam was constructed in 1981; by 1987, the pH had returned to the neutral range in some areas, but dissolved aluminum and manganese concentrations were still at toxic levels, which continued to impede full wildlife recovery. [6] In 1990, Maryland installed lime dosers, devices which dispense alkaline lime into the river, to further mitigate acidity in problem spots. [7] This was successful, and today fish can survive in the river again. [5] : 7
The Potomac River is a major river in the Mid-Atlantic region of the United States that flows from the Potomac Highlands in West Virginia to the Chesapeake Bay in Maryland. It is 405 miles (652 km) long, with a drainage area of 14,700 square miles (38,000 km2), and is the fourth-largest river along the East Coast of the United States and the 21st-largest in the United States. Over 5 million people live within its watershed.
The Tioga River is a tributary of the Chemung River, approximately 58 miles (93 km) long, in northern Pennsylvania and western New York in the United States. It drains a region of ridges in the northern Allegheny Plateau in the watershed of the Susquehanna River.
Jennings Randolph Lake is a reservoir of 952 acres (3.85 km2) located on the North Branch Potomac River in Garrett County, Maryland and Mineral County, West Virginia. It is approximately 8 miles (13 km) upstream of Bloomington, Maryland, and approximately 5 miles (8.0 km) north of Elk Garden, West Virginia.
The Savage River is a 29.5-mile-long (47.5 km) river in Garrett County, Maryland, and is the first major tributary of the North Branch Potomac River from its source. The river was named for 18th-century surveyor John Savage.
Wills Creek is a 38.6-mile-long (62.1 km) tributary of the North Branch Potomac River in Pennsylvania and Maryland in the United States.
Accotink Creek is a 25.0-mile-long (40.2 km) tributary stream of the Potomac River in Fairfax County, Virginia, in the United States. At Springfield, Virginia, Accotink Creek is dammed to create Lake Accotink. The stream empties into the Potomac at Gunston Cove's Accotink Bay, to the west of Fort Belvoir.
Catawissa Creek is a 41.8-mile-long (67.3 km) tributary of the Susquehanna River in east-central Pennsylvania in the United States. Its watershed has an area of 153 square miles (400 km2).
Kettle Creek is a tributary of the West Branch Susquehanna River running through Tioga, Potter, and Clinton counties, in Pennsylvania. It is slightly less than 43 miles (69 km) long. Although many streams in the Kettle Creek watershed are considered "Class A Wild Trout streams" by the Pennsylvania Fish and Boat Commission, the lower reaches of the stream experience acid mine drainage. The upper reaches of the creek are considered to be very high-quality.
Crooked Creek is a 26.3-mile-long (42.3 km) tributary of the Tioga River located entirely in Tioga County, Pennsylvania in the United States.
Pohick Creek is a 14.0-mile-long (22.5 km) tributary stream of the Potomac River in Fairfax County in the U.S. state of Virginia. It takes its name from the Pohick Native American tribe once prevalent in the area.
Evitts Creek is a tributary stream of the North Branch Potomac River in the U.S. states of Pennsylvania and Maryland. The confluence of Evitts Creek and the North Branch Potomac River is located 2 miles (3 km) east of Cumberland, Maryland.
The Maryland Mining Company is a historic coal mining, iron producer and railroad company that operated in Allegany County, Maryland, United States.
The Potomac Wharf Branch was a historic railroad located in Maryland. It was built by the Maryland Mining Company between 1846 and 1850, as an extension to the Eckhart Branch Railroad. The Potomac Wharf Branch crossed Wills Creek on a bridge just east of the present Route 40 road bridge near Cumberland. Rail tracks from this line may still be seen near some billboards, and a gas station in that area.
Dunkard Creek is a stream that flows 36.9 miles (59.4 km) through Greene County, Pennsylvania and Monongalia County, West Virginia, near the towns of Mount Morris, Pennsylvania, and Blacksville, West Virginia. It flows into the Monongahela River northwest of Point Marion, Pennsylvania, approximately three miles north of the Pennsylvania-West Virginia border.
Spring Creek Debris Dam is an earthfill dam on Spring Creek, a tributary of the Sacramento River, in Shasta County in the U.S. state of California. Completed in 1963, the dam, maintained by the U.S. Bureau of Reclamation, serves primarily to collect severe acid mine drainage stemming from the Iron Mountain Mine. The dam forms the Spring Creek Reservoir, less than 1 mile (1.6 km) long. Spring Creek and South Fork Spring Creek flow into the reservoir from a 16-square-mile (41 km2) watershed. The dam is directly upstream from the city of Keswick, California and the Keswick Reservoir. The operation is part of the Trinity River Division of the Central Valley Project.
Drury Run is a tributary of the West Branch Susquehanna River in Clinton County, Pennsylvania, in the United States. It is 7.71 miles (12.41 km) long and its watershed is 11.5 square miles in area, most of which is forest. The stream's tributaries are affected by acid mine drainage, as are the lower reaches of the stream itself. It begins in Tamarack Swamp and flows through Leidy Township, Noyes Township, and Renovo. Brook trout, brown trout, creek chub, and eastern blacknose dace all inhabit the stream.
Seneca Dam was the last in a series of dams proposed on the Potomac River in the area of the Great Falls of the Potomac. Apart from small-scale dams intended to divert water for municipal use in the District of Columbia and into the Chesapeake and Ohio Canal, no version of any scheme was ever built. In most cases the proposed reservoir would have extended upriver to Harpers Ferry, West Virginia. The project was part of a program of as many as sixteen major dams in the Potomac watershed, most of which were never built.
The Potomac River basin reservoir projects were U.S. Army Corps of Engineers programs that sought to regulate the flow of the Potomac River to control flooding, to assure a reliable water supply for Washington, D.C., and to provide recreational opportunities. Beginning in 1921 the Corps studied a variety of proposals for an ambitious program of dam construction on the Potomac and its tributaries, which proposed as many as sixteen major dam and reservoir projects. The most ambitious proposals would have created a nearly continuous chain of reservoirs from tidewater to Cumberland, Maryland. The 1938 program was focused on flood control, on the heels of a major flood in 1936. The reformulated 1963 program focused on water supply and quality, mitigating upstream pollution from sewage and coal mine waste.