North Branch Potomac River

Coordinates: 39°31′42.33″N 078°35′15.05″W / 39.5284250°N 78.5875139°W / 39.5284250; -78.5875139
Source: Wikipedia, the free encyclopedia.
North Branch Potomac River
Tributary to Potomac River
The North Branch between Cumberland, Maryland, and Ridgeley, West Virginia in 2007
North Branch Potomac River is located in West Virginia
North Branch Potomac River
Location of mouth
Location
CountryUnited States
StateWest Virginia, Maryland
CountyAllegany (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
SourceBlackwater River divide
 • locationabout 1 mile northwest of Fairfax, West Virginia
 • coordinates39°11′42.39″N 079°29′21.19″W / 39.1951083°N 79.4892194°W / 39.1951083; -79.4892194[1]
 • elevation2,960 ft (900 m)[1]
MouthPotomac River
 • location
about 1 mile east of Green Spring, West Virginia
 • coordinates
39°31′42.33″N 078°35′15.05″W / 39.5284250°N 78.5875139°W / 39.5284250; -78.5875139[1]
 • elevation
525 ft (160 m)[1]
Length101.27 mi (162.98 km)[2]
Basin size1,343.04 square miles (3,478.5 km2)[3]
Discharge 
 • locationPotomac River
 • average5.13 cu ft/s (0.145 m3/s) at mouth with Potomac River[3]
Basin features
Progression
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.

Course

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.

Water quality

Historically, the North Branch had highly acidic water due to waste from coal mining and paper production in the region.

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 

Tributaries

References

  1. ^ a b c d "Geographic Names Information System". edits.nationalmap.gov. US Geological Survey. Retrieved 7 November 2022.
  2. ^ "ArcGIS Web Application". epa.maps.arcgis.com. US EPA. Retrieved November 6, 2022.
  3. ^ a b "North Branch Potomac River Watershed Report". watersgeo.epa.gov. US EPA. Retrieved 7 November 2022.
  4. ^
    JSTOR 25041735
    .
  5. ^ a b Hansen, Evan; Collins, Alan; Zegre, Sera; Hereford, Anne (December 1, 2010). The Benefits of Acid Mine Drainage Remediation on the North Branch Potomac River (PDF) (Report). Downstream Strategies.
  6. ISSN 1432-1009
    .
  7. ^ Tasker, Greg (November 14, 1993). "Dose of lime may revive dead river; State to neutralize acid mine leaks". The Baltimore Sun.
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