![Potomac River](https://www.english.nina.az/wikipedia/image/aHR0cHM6Ly91cGxvYWQud2lraW1lZGlhLm9yZy93aWtpcGVkaWEvY29tbW9ucy90aHVtYi8wLzBmL0dyZWF0X0ZhbGxzX29mX3RoZV9Qb3RvbWFjX1JpdmVyXy1fTlBTLmpwZy8xNjAwcHgtR3JlYXRfRmFsbHNfb2ZfdGhlX1BvdG9tYWNfUml2ZXJfLV9OUFMuanBn.jpg )
The Potomac River (/pəˈtoʊmək/ ) in the Mid-Atlantic region of the United States flows from the Potomac Highlands in West Virginia to 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. More than 6 million people live within its watershed.
Potomac River | |
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![]() Great Falls of the Potomac River in June 2017 ![]() | |
![]() The Potomac River watershed covers the District of Columbia and parts of four states. | |
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Native name | Patawomeck (Algonquian languages) |
Location | |
Country | United States |
State | West Virginia, Maryland, Virginia, District of Columbia |
Cities | Cumberland, MD; Harpers Ferry, WV; Washington, D.C.; Alexandria, VA |
Physical characteristics | |
Source | North Branch |
• location | Fairfax Stone, Preston County, West Virginia |
• coordinates | 39°11′43″N 79°29′28″W / 39.19528°N 79.49111°W |
• elevation | 3,060 ft (930 m) |
2nd source | South Branch |
• location | Near Monterey, Highland County, Virginia |
• coordinates | 38°25′30″N 79°36′27″W / 38.425°N 79.6075°W |
Source confluence | |
• location | Green Spring, West Virginia |
• coordinates | 39°31′39″N 78°35′15″W / 39.5275°N 78.5875°W |
Mouth | Chesapeake Bay |
• location | St. Mary's County, Maryland/Northumberland County, Virginia, United States |
• coordinates | 38°00′00″N 76°20′06″W / 38°N 76.335°W |
• elevation | 0 ft (0 m) |
Length | 405 mi (652 km) |
Basin size | 14,700 sq mi (38,000 km2) |
Discharge | |
• location | Little Falls, near Washington, D.C. (non-tidal; water years: 1931–2018) |
• average | 11,498 cu ft/s (325.6 m3/s) (1931–2018) |
• minimum | 4,017 cu ft/s (113.7 m3/s) (2002) |
• maximum | 484,000 cu ft/s (13,700 m3/s) (1936) |
Discharge | |
• location | Point of Rocks, Maryland |
• average | 9,504 cu ft/s (269.1 m3/s) |
Discharge | |
• location | Hancock, Maryland |
• average | 4,168 cu ft/s (118.0 m3/s) |
Discharge | |
• location | Paw Paw, West Virginia |
• average | 3,376 cu ft/s (95.6 m3/s) |
Basin features | |
Tributaries | |
• left | Conococheague Creek, Antietam Creek, Monocacy River, Rock Creek, Anacostia River |
• right | Cacapon River, Shenandoah River, Goose Creek, Occoquan River, Wicomico River |
Waterfalls | Great Falls, Little Falls |
Note: Since 1996, the Potomac has been the 'sister river' of the Ara River of Tokyo, Japan |
The river forms part of the borders between Maryland and Washington, D.C., on the left descending bank, and West Virginia and Virginia on the right descending bank. Except for a small portion of its headwaters in West Virginia, the North Branch Potomac River is considered part of Maryland to the low-water mark on the opposite bank. The South Branch Potomac River lies completely within the state of West Virginia except for its headwaters, which lie in Virginia. All navigable parts of the river were designated as a National Recreation Trail in 2006, and the National Oceanic and Atmospheric Administration (NOAA) designated an 18-square-mile (47 km2) portion of the river in Charles County, Maryland, as the Mallows Bay–Potomac River National Marine Sanctuary in 2019.
The river has significant historical and political significance, as the nation's capital of Washington, D.C. is located on its banks, as is Mount Vernon, the home of George Washington. During the American Civil War, the river became the boundary between the Union and the Confederacy, and the Union's largest army, the Army of the Potomac, was named after the river.
Course
The Potomac River runs 405 mi (652 km) from Fairfax Stone Historical Monument State Park in West Virginia on the Allegheny Plateau to Point Lookout, Maryland, and drains 14,679 sq mi (38,020 km2). The length of the river from the junction of its North and South Branches to Point Lookout is 302 mi (486 km).
![image](https://www.english.nina.az/wikipedia/image/aHR0cHM6Ly93d3cuZW5nbGlzaC5uaW5hLmF6L3dpa2lwZWRpYS9pbWFnZS9hSFIwY0hNNkx5OTFjR3h2WVdRdWQybHJhVzFsWkdsaExtOXlaeTkzYVd0cGNHVmthV0V2WTI5dGJXOXVjeTkwYUhWdFlpODFMelZpTDFCb2VYTnBiMmR5WVhCb2FXTmZjSEp2ZG1sdVkyVnpYMjltWDNSb1pWOU5hV1F0UVhSc1lXNTBhV05mY21WbmFXOXVYMko1WDA1UVV5NXdibWN2TWpJd2NIZ3RVR2g1YzJsdlozSmhjR2hwWTE5d2NtOTJhVzVqWlhOZmIyWmZkR2hsWDAxcFpDMUJkR3hoYm5ScFkxOXlaV2RwYjI1ZllubGZUbEJUTG5CdVp3PT0ucG5n.png)
The river has two sources. The source of the North Branch is at the Fairfax Stone located at the junction of Grant, Tucker, and Preston counties in West Virginia. The source of the South Branch is located near Hightown in northern Highland County, Virginia. The river's two branches converge just east of Green Spring in Hampshire County, West Virginia, to form the Potomac. As it flows from its headwaters down to the Chesapeake Bay, the Potomac traverses five geological provinces: the Appalachian Plateau, the Ridge and Valley, the Blue Ridge, the Piedmont Plateau, and the Atlantic coastal plain.
Once the Potomac drops from the Piedmont to the Coastal Plain at the Atlantic Seaboard fall line at Little Falls, tides further influence the river as it passes through Washington, D.C., and beyond. Salinity in the Potomac River Estuary increases thereafter with distance downstream. The estuary also widens, reaching 11 statute miles (17 km) wide at its mouth, between Point Lookout, Maryland, and Smith Point, Virginia, before flowing into the Chesapeake Bay.
Route map of the Potomac River from the confluence of its North and South Branches to the Chesapeake Bay | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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North Branch Potomac River
![image](https://www.english.nina.az/wikipedia/image/aHR0cHM6Ly93d3cuZW5nbGlzaC5uaW5hLmF6L3dpa2lwZWRpYS9pbWFnZS9hSFIwY0hNNkx5OTFjR3h2WVdRdWQybHJhVzFsWkdsaExtOXlaeTkzYVd0cGNHVmthV0V2WTI5dGJXOXVjeTkwYUhWdFlpOHpMek5pTDA1dmNuUm9YMEp5WVc1amFGOVFiM1J2YldGalgxSnBkbVZ5WDBOMWJXSmxjbXhoYm1RdWFuQm5Mekl5TUhCNExVNXZjblJvWDBKeVlXNWphRjlRYjNSdmJXRmpYMUpwZG1WeVgwTjFiV0psY214aGJtUXVhbkJuLmpwZw==.jpg)
The source of the North Branch Potomac River is at the Fairfax Stone located at the junction of Grant, Tucker and Preston counties in West Virginia. From the Fairfax Stone, the North Branch Potomac River flows 27 mi (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.
South Branch Potomac River
The South Branch's source is northwest of Hightown along U.S. Route 250 on the eastern side of Lantz Mountain (3,934 ft) in Highland County. From Hightown, the South Branch is a small meandering stream that flows northeast along Blue Grass Valley Road through the communities of New Hampden and Blue Grass. At Forks of Waters, the South Branch joins with Strait Creek and flows north across the Virginia/West Virginia border into Pendleton County.
The river then travels on a northeastern course along the western side of Jack Mountain (4,045 ft), followed by Sandy Ridge (2,297 ft) along U.S. Route 220. North of the confluence of the South Branch with Smith Creek, the river flows along Town Mountain (2,848 ft) around Franklin at the junction of U.S. Route 220 and U.S. Route 33. After Franklin, the South Branch continues north through the Monongahela National Forest to Upper Tract where it joins with three sizeable streams: Reeds Creek, Mill Run, and Deer Run.
Between Big Mountain (2,582 ft) and Cave Mountain (2,821 ft), the South Branch bends around the Eagle Rock (1,483 ft) outcrop and continues its flow northward into Grant County. Into Grant, the South Branch follows the western side of Cave Mountain through the 20-mile (32 km) long Smoke Hole Canyon, until its confluence with the North Fork at Cabins, where it flows east to Petersburg. At Petersburg, the South Branch Valley Railroad begins, which parallels the river until its mouth at Green Spring.
![image](https://www.english.nina.az/wikipedia/image/aHR0cHM6Ly93d3cuZW5nbGlzaC5uaW5hLmF6L3dpa2lwZWRpYS9pbWFnZS9hSFIwY0hNNkx5OTFjR3h2WVdRdWQybHJhVzFsWkdsaExtOXlaeTkzYVd0cGNHVmthV0V2WTI5dGJXOXVjeTkwYUhWdFlpOHdMekJrTDBoaGJtZHBibWRmVW05amEzTmZWMkZ3Y0c5amIyMXZYMWRXWHpFNE9UQnpMbXB3Wnk4eU1qQndlQzFJWVc1bmFXNW5YMUp2WTJ0elgxZGhjSEJ2WTI5dGIxOVhWbDh4T0Rrd2N5NXFjR2M9LmpwZw==.jpg)
In its eastern course from Petersburg into Hardy County, the South Branch becomes more navigable allowing for canoes and smaller river vessels. The river splits and forms a series of large islands while it heads northeast to Moorefield. At Moorefield, the South Branch is joined by the South Fork South Branch Potomac River and runs north to Old Fields where it is fed by Anderson Run and Stony Run.
At McNeill, the South Branch flows into the Trough where it is bound to its west by Mill Creek Mountain (2,119 ft) and to its east by Sawmill Ridge (1,644 ft). This area is the habitat to bald eagles. The Trough passes into Hampshire County and ends at its confluence with Sawmill Run south of Glebe and Sector.
The South Branch continues north parallel to (County Route 8) toward Romney with a number of historic plantation farms adjoining it. En route to Romney, the river is fed by Buffalo Run, Mill Run, McDowell Run, and Mill Creek at Vanderlip. The South Branch is traversed by the Northwestern Turnpike (U.S. Route 50) and joined by Sulphur Spring Run where it forms Valley View Island to the west of town.
Flowing north of Romney, the river still follows the eastern side of Mill Creek Mountain until it creates a horseshoe bend at Wappocomo's Hanging Rocks around the George W. Washington plantation, Ridgedale. To the west of Three Churches on the western side of South Branch Mountain, 3,028 feet (923 m), the South Branch creates a series of bends and flows to the northeast by Springfield through Blue's Ford. After two additional horseshoe bends (meanders), the South Branch flows under the old Baltimore and Ohio Railroad mainline between Green Spring and South Branch Depot, and joins the North Branch to form the Potomac.
Upper Potomac River
This stretch encompasses the section of the Potomac River from the confluence of its North and South Branches through Opequon Creek near Shepherdstown, West Virginia. Along the way the following tributaries drain into the Potomac: North Branch Potomac River, South Branch Potomac River, Town Creek, Little Cacapon River, Sideling Hill Creek, Cacapon River, Sir Johns Run, Warm Spring Run, Tonoloway Creek, Fifteenmile Creek, Sleepy Creek, Cherry Run, Back Creek, Conococheague Creek, and Opequon Creek.
Lower Potomac River
![image](https://www.english.nina.az/wikipedia/image/aHR0cHM6Ly93d3cuZW5nbGlzaC5uaW5hLmF6L3dpa2lwZWRpYS9pbWFnZS9hSFIwY0hNNkx5OTFjR3h2WVdRdWQybHJhVzFsWkdsaExtOXlaeTkzYVd0cGNHVmthV0V2WTI5dGJXOXVjeTkwYUhWdFlpODJMelkwTDBGbGNtbGhiRjlRYUc5MGIxOXZabDlJWVhKd1pYSnpYMFpsY25KNVh5VXlPREUxTmpRMk56a3dORGN6SlRJNUxtcHdaeTh5TWpCd2VDMUJaWEpwWVd4ZlVHaHZkRzlmYjJaZlNHRnljR1Z5YzE5R1pYSnllVjhsTWpneE5UWTBOamM1TURRM015VXlPUzVxY0djPS5qcGc=.jpg)
This section covers the Potomac from just above Harpers Ferry in West Virginia down to Little Falls, Maryland on the border between Maryland and Washington, DC. Along the way the following tributaries drain into the Potomac: Antietam Creek, Shenandoah River, Catoctin Creek (Virginia), Catoctin Creek (Maryland), Tuscarora Creek, Monocacy River, Little Monocacy River, Broad Run, Goose Creek, Broad Run, Horsepen Branch, Little Seneca Creek, Tenmile Creek, Great Seneca Creek, Old Sugarland Run, Muddy Branch, Nichols Run, Watts Branch, Limekiln Branch, Carroll Branch, Pond Run, Clarks Branch, Mine Run Branch, Difficult Run, Bullneck Run, Rock Run, Scott Run, Dead Run, Turkey Run, Cabin John Creek, Minnehaha Branch, and Little Falls Branch.
Tidal Potomac River
![image](https://www.english.nina.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.jpg)
The Tidal Potomac River lies below the Fall Line. This 108-mile (174-km) stretch encompasses the Potomac from a short distance below the Washington, DC - Montgomery County line, just downstream of the Little Falls of the Potomac River, to the Chesapeake Bay. Along the way the following tributaries drain into the Potomac: Pimmit Run, Gulf Branch, Donaldson Run, Windy Run, Spout Run, Maddox Branch, Foundry Branch, Rock Creek, Rocky Run, Tiber Creek, Roaches Run, Washington Channel, Anacostia River, Four Mile Run, Oxon Creek, Hunting Creek, , Henson Creek, Swan Creek, Piscataway Creek, Little Hunting Creek, Dogue Creek, Accotink Creek, Pohick Creek, Pomonkey Creek, Occoquan River, Neabsco Creek, Powell's Creek, Mattawoman Creek, , Quantico Creek, , Chopawamsic Creek, , Aquia Creek, Potomac Creek, Nanjemoy Creek, , Port Tobacco River, Popes Creek, , Clifton Creek, , , Wicomico River, , , Mattox Creek, Popes Creek, , St. Marys River, Yeocomico River, Coan River, and Hull Creek.
History
Natural history
The river itself is at least 3.5 million years old, likely extending back ten to twenty million years before the present when the Atlantic Ocean lowered and exposed coastal sediments along the fall line. This included the area at Great Falls, which eroded into its present form during recent glaciation periods.
The stream gradient of the entire river is 0.14%, a drop of 930 m over 652 km.
Human history
![image](https://www.english.nina.az/wikipedia/image/aHR0cHM6Ly93d3cuZW5nbGlzaC5uaW5hLmF6L3dpa2lwZWRpYS9pbWFnZS9hSFIwY0hNNkx5OTFjR3h2WVdRdWQybHJhVzFsWkdsaExtOXlaeTkzYVd0cGNHVmthV0V2WTI5dGJXOXVjeTkwYUhWdFlpOWhMMkZrTDBSbGRHRnBiRjl2Wmw4eE5qQTRYMU50YVhSb1gwMWhjRjl6YUc5M2FXNW5YM1JvWlY5UVlYUmhkMjl0WldOclgxSnBkbVZ5TG1wd1p5OHlNakJ3ZUMxRVpYUmhhV3hmYjJaZk1UWXdPRjlUYldsMGFGOU5ZWEJmYzJodmQybHVaMTkwYUdWZlVHRjBZWGR2YldWamExOVNhWFpsY2k1cWNHYz0uanBn.jpg)
"Potomac" is a European spelling of Patawomeck, the Algonquian name of a Native American village on its southern bank. Native Americans had different names for different parts of the river, calling the river above Great Falls Cohongarooton, meaning "honking geese" and "Patawomke" below the Falls, meaning "river of swans". In 1608, Captain John Smith explored the river now known as the Potomac and made drawings of his observations which were later compiled into a map and published in London in 1612. This detail from that map shows his rendition of the river that the local tribes had told him was called the "Patawomeck". The spelling of the name has taken many forms over the years from "Patawomeck" (as on Captain John Smith's map) to "Patomake", "Patowmack", and numerous other variations in the 18th century and now "Potomac". The river's name was officially decided upon as "Potomac" by the Board on Geographic Names in 1931.
![image](https://www.english.nina.az/wikipedia/image/aHR0cHM6Ly93d3cuZW5nbGlzaC5uaW5hLmF6L3dpa2lwZWRpYS9pbWFnZS9hSFIwY0hNNkx5OTFjR3h2WVdRdWQybHJhVzFsWkdsaExtOXlaeTkzYVd0cGNHVmthV0V2WTI5dGJXOXVjeTkwYUhWdFlpODRMemcwTDFSMWJtUnlZVjl6ZDJGdWMxOGxNamcyTlRZMU9UZ3pOREk1SlRJNUxtcHdaeTh5TWpCd2VDMVVkVzVrY21GZmMzZGhibk5mSlRJNE5qVTJOVGs0TXpReU9TVXlPUzVxY0djPS5qcGc=.jpg)
The similarity of the name to the Ancient Greek word for river, potamos, has been noted for more than two centuries but it appears to be due to chance.
The Potomac River brings together a variety of cultures throughout the watershed from the coal miners of upstream West Virginia to the urban residents of the nation's capital and, along the lower Potomac, the watermen of Virginia's Northern Neck.
![image](https://www.english.nina.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.jpg)
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Top row: Chain Bridge (two views) and Pimmit Run Bridge; Bottom Row: Aqueduct Bridget {two views) and Georgetown Ferry
Being situated in an area rich in American history and American heritage has led to the Potomac being nicknamed "the Nation's River". George Washington, the first President of the United States, was born in, surveyed, and spent most of his life within, the Potomac basin. All of Washington, D.C., the nation's capital city, also lies within the watershed. The First United States Congress by act of July 16, 1790 stated that the nation's capital was to be located on the river. The 1859 siege of Harper's Ferry at the river's confluence with the Shenandoah was a precursor to numerous epic battles of the American Civil War in and around the Potomac and its tributaries, such as the 1861 Battle of Ball's Bluff and the 1862 Battle of Shepherdstown.
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General Robert E. Lee crossed the river, thereby invading the North and threatening Washington, D.C., twice in campaigns climaxing in the battles of Antietam (September 17, 1862) and Gettysburg (July 1–3, 1863). Confederate General Jubal Early crossed the river in July 1864 on his attempted raid on the nation's capital. The river not only divided the Union from the Confederacy, but also gave name to the Union's largest army, the Army of the Potomac. The Patowmack Canal was intended by George Washington to connect the Tidewater region near Georgetown with Cumberland, Maryland. Started in 1785 on the Virginia side of the river, it was not completed until 1802. Financial troubles led to the closure of the canal in 1830. The Chesapeake and Ohio Canal operated along the banks of the Potomac in Maryland from 1831 to 1924 and also connected Cumberland to Washington, D.C. This allowed freight to be transported around the rapids known as the Great Falls of the Potomac River, as well as many other, smaller rapids.
Washington, D.C. began using the Potomac as its principal source of drinking water with the opening of the Washington Aqueduct in 1864, using a water intake constructed at Great Falls.
Hydrology
Water supply and water quality
An average of approximately 486 million US gallons (1,840,000 m3) of water is withdrawn daily from the Potomac in the Washington area for water supply, providing about 78 percent of the region's total water usage, this amount includes approximately 80 percent of the drinking water consumed by the region's estimated 6.1 million residents.
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As a result of damaging floods in 1936 and 1937, the Army Corps of Engineers proposed the Potomac River basin reservoir projects, a series of dams that were intended to regulate the river and to provide a more reliable water supply. One dam was to be built at Little Falls, just north of Washington, backing its pool up to Great Falls. Just above Great Falls, the much larger Seneca Dam was proposed whose reservoir would extend to Harpers Ferry. Several other dams were proposed for the Potomac and its tributaries.
Dams on the Potomac River |
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When detailed studies were issued by the Corps in the 1950s, they met sustained opposition, led by U.S. Supreme Court Justice William O. Douglas, resulting in the plans' abandonment. The only dam project that did get built was Jennings Randolph Lake on the North Branch. The Corps built a supplementary water intake for the Washington Aqueduct at Little Falls in 1959.
In 1940 Congress passed a law authorizing the creation of an interstate compact to coordinate water quality management among states in the Potomac basin. Maryland, West Virginia, Pennsylvania, Virginia, and the District of Columbia agreed to establish the Interstate Commission on the Potomac River Basin. The compact was amended in 1970 to include coordination of water supply issues and land use issues related to water quality.
Beginning in the 19th century, with increasing mining and agriculture upstream and urban sewage and runoff downstream, the water quality of the Potomac River deteriorated. This created conditions of severe eutrophication. It is said that President Abraham Lincoln used to escape to the highlands on summer nights to escape the river's stench. In the 1960s, with dense green algal blooms covering the river's surface, President Lyndon Johnson declared the river "a national disgrace" and set in motion a long-term effort to reduce pollution from sewage and restore the beauty and ecology of this historic river. One of the significant pollution control projects at the time was the expansion of the Blue Plains Advanced Wastewater Treatment Plant, which serves Washington and several surrounding communities. Enactment of the 1972 Clean Water Act led to construction or expansion of additional sewage treatment plants in the Potomac watershed. Controls on phosphorus, one of the principal contributors to eutrophication, were implemented in the 1980s, through sewage plant upgrades and restrictions on phosphorus in detergents.
By the end of the 20th century, notable success had been achieved, as massive algal blooms vanished and recreational fishing and boating rebounded. Still, the aquatic habitat of the Potomac River and its tributaries remain vulnerable to eutrophication, heavy metals, pesticides and other toxic chemicals, over-fishing, alien species, and pathogens associated with fecal coliform bacteria and shellfish diseases. In 2005 two federal agencies, the US Geological Survey and the Fish and Wildlife Service, began to identify fish in the Potomac and tributaries that exhibited "intersex" characteristics, as a result of endocrine disruption caused by some form of pollution.
On November 13, 2007, the Potomac Conservancy, an environmental group, issued the river a grade of "D-plus", citing high levels of pollution and the reports of "intersex" fish. Since then, the river has improved with a reduction in nutrient runoff, return of fish populations, and land protection along the river. As a result, the same group issued a grade of "B" for 2017 and 2018. In March 2019, the Potomac Riverkeeper Network launched a laboratory boat dubbed the "Sea Dog", which will be monitoring water quality in the Potomac and providing reports to the public on a weekly basis; in that same month, the catching near Fletcher's Boat House of a Striped Bass estimated to weigh 35 lb (16 kg) was seen as a further indicator of the continuing improvement in the health of the river.
Top Ten Historic Crests of the Potomac River, 1877–2017 | |||||||
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Kitzmiller | Hancock | Williamsport | Shepherdstown | ||||
Harpers Ferry | Point of Rocks | Little Falls | Georgetown | ||||
Source: National Weather Service |
Discharge
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The average daily flow during the water years 1931–2018 was 11,498 cubic feet (325.6 m3) /s. The highest average daily flow ever recorded on the Potomac at Little Falls, Maryland (near Washington, D.C.), was in March 1936 when it reached 426,000 cubic feet (12,100 m3) /s. The lowest average daily flow ever recorded at the same location was 601.0 cubic feet (17.02 m3) /s in September 1966 The highest crest of the Potomac ever registered at Little Falls was 28.10 ft, on March 19, 1936; however, the most damaging flood to affect Washington, DC and its metropolitan area was that of October 1942.
Legal issues
For 400 years Maryland and Virginia have disputed control of the Potomac and its North Branch since both states' original colonial charters grant the entire river rather than half of it as is normally the case with boundary rivers. In its first state constitution adopted in 1776, Virginia ceded its claim to the entire river but reserved free use of it, an act disputed by Maryland. Both states acceded to the 1785 Mount Vernon Compact and the 1877 Black-Jenkins Award which granted Maryland the river bank-to-bank from the low-water mark on the Virginia side while permitting Virginia full riparian rights short of obstructing navigation.
From 1957 to 1996, the Maryland Department of the Environment (MDE) routinely issued permits applied for by Virginia entities concerning the use of the Potomac. However, in 1996 the MDE denied a permit submitted by the Fairfax County Water Authority to build a water intake 725 feet (220 m) offshore, citing potential harm to Maryland's interests by an increase in Virginia sprawl caused by the project. After years of failed appeals within the Maryland government's appeal processes, in 2000 Virginia took the case to the Supreme Court of the United States, which exercises original jurisdiction in cases between two states. Maryland claimed Virginia lost its riparian rights by acquiescing to MDE's permit process for 63 years (MDE began its permit process in 1933). A Special Master appointed by the Supreme Court to investigate recommended the case be settled in favor of Virginia, citing the language in the 1785 Compact and the 1877 Award. On December 9, 2003, the Court agreed in a 7–2 decision.
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The original charters are silent as to which branch from the upper Potomac serves as the boundary, but this was settled by the 1785 Compact. When West Virginia seceded from Virginia in 1863, the question of West Virginia's succession in title to the lands between the branches of the river was raised, as well as title to the river itself. Claims by Maryland to West Virginia land north of the South Branch (all of Mineral and Grant Counties and parts of Hampshire, Hardy, Tucker and Pendleton Counties) and by West Virginia to the Potomac's high-water mark were rejected by the Supreme Court in two separate decisions in 1910.
Fauna
Fish
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A variety of fish inhabit the Potomac, including bass, muskellunge, pike, walleye. The northern snakehead, an invasive species resembling the native bowfin, lamprey, and American eel, was first seen in 2004. Many species of sunfish are also present in the Potomac and its headwaters. Although rare, bull sharks can be found.
After having been depressed for many decades, the river's population of American shad is currently re-bounding as a result of the ICPRB's successful "American Shad Restoration Project" that was begun in 1995. In addition to stocking the river with more than 22 million shad fry, the Project supervised the construction of a fishway that was built to facilitate the passage of adults around the Little Falls Dam on the way to their traditional spawning grounds upstream.
Freshwater fish of the Potomac River |
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Tidal freshwater fish of the Potomac River |
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Mammals
Mammals of the Potomac River Basin |
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Early European colonists who settled along the Potomac found a diversity of large and small mammals living in the dense forests nearby. Bison, elk, wolves (both gray and red) and cougars were still present at that time, but had been hunted to extirpation by the middle of the 19th century. Among the denizens of the Potomac's banks, beavers and otters met a similar fate, while small populations of American mink and American martens survived into the 20th century in some secluded areas.
There is no record of early settlers having observed marine mammals in the Potomac, but several sightings of Atlantic bottle-nosed dolphins (Tursiops truncatus) were reported during the 19th century. In July 1844, a pod of 14 adults and young was followed up the river by men in boats as high as the Aqueduct Bridge (approximately the same location occupied by Key Bridge today).
Since 2015, perhaps as a result of warmer temperatures, rising water levels in the Chesapeake Bay and improving water quality in the Potomac, unprecedented numbers of Atlantic bottle-nosed dolphins have been observed in the river. According to Dr. Janet Mann of Georgetown University's Potomac-Chesapeake Dolphin Project, more than 500 individual members of the species have been identified in the Potomac during this period.
Birds
Birds of the Potomac River Basin |
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Reptiles
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Turtles of the Potomac River Basin |
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Snakes of the Potomac River basin |
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Lizards of the Potomac River Basin |
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Amphibians
Salamanders of the Potomac River Basin |
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Frogs and toads of the Potomac River Basin |
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Additional images
- Upper and lower Potomac
- The South Branch near South Branch Depot, West Virginia
- Confluence of the Cacapon River (barely visible) with the Potomac
- Oblique air photo, facing southwest, of the Potomac River flowing through water gaps in the Blue Ridge Mountains. Virginia on the left, Maryland on the right, West Virginia in upper right, including Harpers Ferry (partially obscured by Maryland Heights of Elk Ridge Mountain) at the confluence of the Potomac and Shenandoah Rivers.
- Potomac River at Goose Creek
- The Great Falls of the Potomac, viewed from the Virginia bank of the river (Engraving based on an aquatint drawn by George Jacob Beck in 1802)
- Tidal Potomac
- Potomac near Occoquan Bay
- View of the Potomac River, Analostan Island, Georgetown, and, in the distance, buildings of the nascent City of Washington. (Engraving based on an 1801 watercolor by George Jacob Beck.)
- Jefferson Memorial in Washington, D.C., viewed from across the Tidal Basin of the Potomac
- The Pentagon, looking northeast with the Potomac in the distance
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The Potomac River p e ˈ t oʊ m e k in the Mid Atlantic region of the United States flows from the Potomac Highlands in West Virginia to 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 More than 6 million people live within its watershed Potomac RiverGreat Falls of the Potomac River in June 2017The Potomac River watershed covers the District of Columbia and parts of four states Native namePatawomeck Algonquian languages LocationCountryUnited StatesStateWest Virginia Maryland Virginia District of ColumbiaCitiesCumberland MD Harpers Ferry WV Washington D C Alexandria VAPhysical characteristicsSourceNorth Branch locationFairfax Stone Preston County West Virginia coordinates39 11 43 N 79 29 28 W 39 19528 N 79 49111 W 39 19528 79 49111 elevation3 060 ft 930 m 2nd sourceSouth Branch locationNear Monterey Highland County Virginia coordinates38 25 30 N 79 36 27 W 38 425 N 79 6075 W 38 425 79 6075Source confluence locationGreen Spring West Virginia coordinates39 31 39 N 78 35 15 W 39 5275 N 78 5875 W 39 5275 78 5875MouthChesapeake Bay locationSt Mary s County Maryland Northumberland County Virginia United States coordinates38 00 00 N 76 20 06 W 38 N 76 335 W 38 76 335 elevation0 ft 0 m Length405 mi 652 km Basin size14 700 sq mi 38 000 km2 Discharge locationLittle Falls near Washington D C non tidal water years 1931 2018 average11 498 cu ft s 325 6 m3 s 1931 2018 minimum4 017 cu ft s 113 7 m3 s 2002 maximum484 000 cu ft s 13 700 m3 s 1936 Discharge locationPoint of Rocks Maryland average9 504 cu ft s 269 1 m3 s Discharge locationHancock Maryland average4 168 cu ft s 118 0 m3 s Discharge locationPaw Paw West Virginia average3 376 cu ft s 95 6 m3 s Basin featuresTributaries leftConococheague Creek Antietam Creek Monocacy River Rock Creek Anacostia River rightCacapon River Shenandoah River Goose Creek Occoquan River Wicomico RiverWaterfallsGreat Falls Little FallsNote Since 1996 the Potomac has been the sister river of the Ara River of Tokyo Japan The river forms part of the borders between Maryland and Washington D C on the left descending bank and West Virginia and Virginia on the right descending bank Except for a small portion of its headwaters in West Virginia the North Branch Potomac River is considered part of Maryland to the low water mark on the opposite bank The South Branch Potomac River lies completely within the state of West Virginia except for its headwaters which lie in Virginia All navigable parts of the river were designated as a National Recreation Trail in 2006 and the National Oceanic and Atmospheric Administration NOAA designated an 18 square mile 47 km2 portion of the river in Charles County Maryland as the Mallows Bay Potomac River National Marine Sanctuary in 2019 The river has significant historical and political significance as the nation s capital of Washington D C is located on its banks as is Mount Vernon the home of George Washington During the American Civil War the river became the boundary between the Union and the Confederacy and the Union s largest army the Army of the Potomac was named after the river CourseThe Potomac River in Washington D C with Arlington Memorial Bridge in the foreground and Rosslyn Arlington Virginia in the background The Potomac River runs 405 mi 652 km from Fairfax Stone Historical Monument State Park in West Virginia on the Allegheny Plateau to Point Lookout Maryland and drains 14 679 sq mi 38 020 km2 The length of the river from the junction of its North and South Branches to Point Lookout is 302 mi 486 km Map showing the five geological provinces through which the Potomac River flows The river has two sources The source of the North Branch is at the Fairfax Stone located at the junction of Grant Tucker and Preston counties in West Virginia The source of the South Branch is located near Hightown in northern Highland County Virginia The river s two branches converge just east of Green Spring in Hampshire County West Virginia to form the Potomac As it flows from its headwaters down to the Chesapeake Bay the Potomac traverses five geological provinces the Appalachian Plateau the Ridge and Valley the Blue Ridge the Piedmont Plateau and the Atlantic coastal plain Once the Potomac drops from the Piedmont to the Coastal Plain at the Atlantic Seaboard fall line at Little Falls tides further influence the river as it passes through Washington D C and beyond Salinity in the Potomac River Estuary increases thereafter with distance downstream The estuary also widens reaching 11 statute miles 17 km wide at its mouth between Point Lookout Maryland and Smith Point Virginia before flowing into the Chesapeake Bay vteRoute map of the Potomac River from the confluence of its North and South Branches to the Chesapeake BayLegendNorth Branch Potomac River West VirginiaMarylandSouth Branch Potomac RiverTown CreekLittle Cacapon RiverFifteenmile CreekPaw Paw Bridge WV 9 MD 51Sideling Hill CreekCacapon RiverSir Johns RunGrasshopper RunHancock Bridge US 522Warm Spring RunTonoloway CreekSleepy CreekLicking CreekCherry RunBack CreekLittle Conococheague CreekConococheague CreekWilliamsport Pike Bridge US 11Maryland Veterans Memorial Bridge I 81Opequon CreekRumsey Shepherdstown Bridge WV 480 MD 34Rattlesnake RunPackhorse FordAntietam Creek The Needles RapidsShenandoah RiverPotomac Water Gap between Blue Ridge Mt VA WV and Elk Ridge Mt MD Harpers Ferry Whitewater PoolWhite Horse RapidsWest VirginiaVirginiaPotomac Water Gap between Short Hill Mt VA and South Mt MD Sandy Hook Bridge US 340Israel CreekBrunswick Bridge SR 287 MD 17Catoctin CreekLittle Catoctin CreekCatoctin CreekPotomac Water Gap between Furnace Mt VA and Pine Rock MD Point of Rocks Bridge US 15Heaters Island WMA MD White s FordNolands Ferry historic Tuscarora CreekCheek s FordMonocacy RiverLittle Monocacy RiverMason Island WMA MD White s Ferry SR 655 MD 107Ball s Bluff VA and Harrison Island MD Broad RunEdwards Ferry historic Goose CreekSelden Island MD Broad RunHorsepen CreekHorsepen BranchMcKee Beshers Wildlife MGT AreaSharpshin Island MD Sugarland RunRowsers FordSeneca Redstone Quarry historic Seneca CreekBlockhouse Point PromontoryMuddy BranchNichols RunWatts BranchGladys Island Potomac River MD Cool Spring BranchConn s Ferry historic Conn Island Potomac River MD Limekiln Branch supplies water to the Washington Aqueduct AQU Beginning of Potomac GorgeGreat FallsCarroll BranchOlmsted Island formerly Great Falls Island MD boulders and sediment left by the ancestral Potomac River GHL Mine Run BranchBear Island and Billy Goat Trail Section A Maryland Sherwin Island formerly Cupid s Bower Island MD Rocky Island s and Hidden Gorge MD Ruins of MatildavilleBeginning of Mather Gorge boat ramp take out only Difficult RunCow Hoof Rock and Black Pond site of most recent paleo falls gt 30 kya BLK VA Offutt Island MD Bullneck RunRock RunTurkey Island MD Scott s RunScott s Run Nature Preserveand Knickpoint paleo falls 200 kya End of Mather GorgeAmerican Legion Cabin John Bridge I 495Capital BeltwayPlummers Island MD Plummers Island Thrust Fault inactive PIF Dead RunTurkey Run Potomac River Cabin John CreekMinnehaha BranchSycamore Island MD Little Falls Dam and Dalecarlia ReservoirLittle FallsLittle Falls BranchMarylandDistrict of ColumbiaWestern boundary of the Atlantic Seaboard fall line Potomac Estuary begins PES Chain Bridge SR 123 and Canal Road Clara Barton PkwyPimmit RunGulf BranchDonaldson RunWindy RunSpout RunMaddox BranchThree Sisters IslandFoundry BranchRuins of Aqueduct BridgeFrancis Scott Key Bridge US 29Rock CreekEnd of Potomac GorgeLimit of navigation Eastern boundary of the Atlantic Seaboard fall lineTheodore Roosevelt Island TRI DC Theodore Roosevelt Bridge I 66 US 50 paved over Columbia Island DC Arlington Memorial BridgeTidal Basin and Washington ChannelGeorge Mason Memorial Bridge I 395 south US 1 southRochambeau Memorial Bridge I 395HOV US 1Arland D Williams Jr Memorial Bridge I 395 north US 1 northRoaches Run Waterfowl SanctuaryTiber Creek paved over Hains PointAnacostia RiverFour Mile RunOxon CreekDistrict of ColumbiaMarylandWoodrow Wilson Bridge I 95 I 495Capital BeltwayJones Point LightHunting CreekDyke Marsh Wildlife PreserveBroad CreekHenson CreekSwan CreekPiscataway CreekLittle Hunting CreekMount Vernon EstateDogue CreekAccotink CreekPohick CreekPomonkey CreekMason Neck Wildlife RefugeOccoquan RiverFeatherstone National Wildlife RefugeNeabsco CreekPowells CreekMattawoman CreekChicamuxen CreekQuantico CreekChopawamsic Island VA Chopawamsic CreekTank CreekAquia CreekCrow s Nest Natural Area PreservePotomac CreekNanjemoy CreekChotank CreekPort Tobacco RiverPopes CreekGambo CreekClifton CreekGovernor Harry W Nice Memorial Bridge US 301Piccowaxen CreekUpper Machodoc CreekWicomico RiverCobb Island MD St Clement s Island MD Monroe CreekMattox CreekPopes CreekSt Marys RiverYeocomico RiverCoan RiverHull CreekPoint Lookout LightSmith Point LightDebouchment of the Potomac EstuaryChesapeake Bay North Branch Potomac River The North Branch between Cumberland Maryland and Ridgeley West Virginia in 2007 The source of the North Branch Potomac River is at the Fairfax Stone located at the junction of Grant Tucker and Preston counties in West Virginia From the Fairfax Stone the North Branch Potomac River flows 27 mi 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 South Branch Potomac River The South Branch s source is northwest of Hightown along U S Route 250 on the eastern side of Lantz Mountain 3 934 ft in Highland County From Hightown the South Branch is a small meandering stream that flows northeast along Blue Grass Valley Road through the communities of New Hampden and Blue Grass At Forks of Waters the South Branch joins with Strait Creek and flows north across the Virginia West Virginia border into Pendleton County The river then travels on a northeastern course along the western side of Jack Mountain 4 045 ft followed by Sandy Ridge 2 297 ft along U S Route 220 North of the confluence of the South Branch with Smith Creek the river flows along Town Mountain 2 848 ft around Franklin at the junction of U S Route 220 and U S Route 33 After Franklin the South Branch continues north through the Monongahela National Forest to Upper Tract where it joins with three sizeable streams Reeds Creek Mill Run and Deer Run Between Big Mountain 2 582 ft and Cave Mountain 2 821 ft the South Branch bends around the Eagle Rock 1 483 ft outcrop and continues its flow northward into Grant County Into Grant the South Branch follows the western side of Cave Mountain through the 20 mile 32 km long Smoke Hole Canyon until its confluence with the North Fork at Cabins where it flows east to Petersburg At Petersburg the South Branch Valley Railroad begins which parallels the river until its mouth at Green Spring Canoeists at Hanging Rocks on the South Branch in the 1890s In its eastern course from Petersburg into Hardy County the South Branch becomes more navigable allowing for canoes and smaller river vessels The river splits and forms a series of large islands while it heads northeast to Moorefield At Moorefield the South Branch is joined by the South Fork South Branch Potomac River and runs north to Old Fields where it is fed by Anderson Run and Stony Run At McNeill the South Branch flows into the Trough where it is bound to its west by Mill Creek Mountain 2 119 ft and to its east by Sawmill Ridge 1 644 ft This area is the habitat to bald eagles The Trough passes into Hampshire County and ends at its confluence with Sawmill Run south of Glebe and Sector The South Branch continues north parallel to County Route 8 toward Romney with a number of historic plantation farms adjoining it En route to Romney the river is fed by Buffalo Run Mill Run McDowell Run and Mill Creek at Vanderlip The South Branch is traversed by the Northwestern Turnpike U S Route 50 and joined by Sulphur Spring Run where it forms Valley View Island to the west of town Flowing north of Romney the river still follows the eastern side of Mill Creek Mountain until it creates a horseshoe bend at Wappocomo s Hanging Rocks around the George W Washington plantation Ridgedale To the west of Three Churches on the western side of South Branch Mountain 3 028 feet 923 m the South Branch creates a series of bends and flows to the northeast by Springfield through Blue s Ford After two additional horseshoe bends meanders the South Branch flows under the old Baltimore and Ohio Railroad mainline between Green Spring and South Branch Depot and joins the North Branch to form the Potomac Upper Potomac River This stretch encompasses the section of the Potomac River from the confluence of its North and South Branches through Opequon Creek near Shepherdstown West Virginia Along the way the following tributaries drain into the Potomac North Branch Potomac River South Branch Potomac River Town Creek Little Cacapon River Sideling Hill Creek Cacapon River Sir Johns Run Warm Spring Run Tonoloway Creek Fifteenmile Creek Sleepy Creek Cherry Run Back Creek Conococheague Creek and Opequon Creek Lower Potomac River Confluence of the Potomac and Shenandoah at Harpers Ferry This section covers the Potomac from just above Harpers Ferry in West Virginia down to Little Falls Maryland on the border between Maryland and Washington DC Along the way the following tributaries drain into the Potomac Antietam Creek Shenandoah River Catoctin Creek Virginia Catoctin Creek Maryland Tuscarora Creek Monocacy River Little Monocacy River Broad Run Goose Creek Broad Run Horsepen Branch Little Seneca Creek Tenmile Creek Great Seneca Creek Old Sugarland Run Muddy Branch Nichols Run Watts Branch Limekiln Branch Carroll Branch Pond Run Clarks Branch Mine Run Branch Difficult Run Bullneck Run Rock Run Scott Run Dead Run Turkey Run Cabin John Creek Minnehaha Branch and Little Falls Branch Tidal Potomac River View southwest across the tidal Potomac River from the south end of Cobb Island Road on Cobb Island Charles County Maryland The Tidal Potomac River lies below the Fall Line This 108 mile 174 km stretch encompasses the Potomac from a short distance below the Washington DC Montgomery County line just downstream of the Little Falls of the Potomac River to the Chesapeake Bay Along the way the following tributaries drain into the Potomac Pimmit Run Gulf Branch Donaldson Run Windy Run Spout Run Maddox Branch Foundry Branch Rock Creek Rocky Run Tiber Creek Roaches Run Washington Channel Anacostia River Four Mile Run Oxon Creek Hunting Creek Henson Creek Swan Creek Piscataway Creek Little Hunting Creek Dogue Creek Accotink Creek Pohick Creek Pomonkey Creek Occoquan River Neabsco Creek Powell s Creek Mattawoman Creek Quantico Creek Chopawamsic Creek Aquia Creek Potomac Creek Nanjemoy Creek Port Tobacco River Popes Creek Clifton Creek Wicomico River Mattox Creek Popes Creek St Marys River Yeocomico River Coan River and Hull Creek HistoryNatural history The river itself is at least 3 5 million years old likely extending back ten to twenty million years before the present when the Atlantic Ocean lowered and exposed coastal sediments along the fall line This included the area at Great Falls which eroded into its present form during recent glaciation periods The stream gradient of the entire river is 0 14 a drop of 930 m over 652 km Human history Captain John Smith s 1608 map Potomac is a European spelling of Patawomeck the Algonquian name of a Native American village on its southern bank Native Americans had different names for different parts of the river calling the river above Great Falls Cohongarooton meaning honking geese and Patawomke below the Falls meaning river of swans In 1608 Captain John Smith explored the river now known as the Potomac and made drawings of his observations which were later compiled into a map and published in London in 1612 This detail from that map shows his rendition of the river that the local tribes had told him was called the Patawomeck The spelling of the name has taken many forms over the years from Patawomeck as on Captain John Smith s map to Patomake Patowmack and numerous other variations in the 18th century and now Potomac The river s name was officially decided upon as Potomac by the Board on Geographic Names in 1931 Tundra swans were the predominant species of swan on the Potomac River when the Algonquian tribes dwelled along its shores and continue to be the most populous variety today The similarity of the name to the Ancient Greek word for river potamos has been noted for more than two centuries but it appears to be due to chance The Potomac River brings together a variety of cultures throughout the watershed from the coal miners of upstream West Virginia to the urban residents of the nation s capital and along the lower Potomac the watermen of Virginia s Northern Neck View of the Potomac River from George Washington s birthplace in Westmoreland County VirginiaThe Potomac running next to the Lincoln Memorial and under the Arlington Memorial BridgeCivil War EraConfederate troops crossing the fords of the Potomac in early September 1862 for the invasion of Maryland which would culminate in the Battle of Antietam Print of a wood carving based on a drawing by Thomas Nast first published in the September 27 1862 edition of Harper s Weekly Union defenses along the Potomac near Washington DC Top row Chain Bridge two views and Pimmit Run Bridge Bottom Row Aqueduct Bridget two views and Georgetown FerryUnion soldiers manning the Lower Battery at the north end of Chain Bridge in 1862Union soldiers on the Potomac River across from Georgetown University in 1861 Being situated in an area rich in American history and American heritage has led to the Potomac being nicknamed the Nation s River George Washington the first President of the United States was born in surveyed and spent most of his life within the Potomac basin All of Washington D C the nation s capital city also lies within the watershed The First United States Congress by act of July 16 1790 stated that the nation s capital was to be located on the river The 1859 siege of Harper s Ferry at the river s confluence with the Shenandoah was a precursor to numerous epic battles of the American Civil War in and around the Potomac and its tributaries such as the 1861 Battle of Ball s Bluff and the 1862 Battle of Shepherdstown Map of the Potomac River and its environs c 1862 by Robert Knox Sneden General Robert E Lee crossed the river thereby invading the North and threatening Washington D C twice in campaigns climaxing in the battles of Antietam September 17 1862 and Gettysburg July 1 3 1863 Confederate General Jubal Early crossed the river in July 1864 on his attempted raid on the nation s capital The river not only divided the Union from the Confederacy but also gave name to the Union s largest army the Army of the Potomac The Patowmack Canal was intended by George Washington to connect the Tidewater region near Georgetown with Cumberland Maryland Started in 1785 on the Virginia side of the river it was not completed until 1802 Financial troubles led to the closure of the canal in 1830 The Chesapeake and Ohio Canal operated along the banks of the Potomac in Maryland from 1831 to 1924 and also connected Cumberland to Washington D C This allowed freight to be transported around the rapids known as the Great Falls of the Potomac River as well as many other smaller rapids Washington D C began using the Potomac as its principal source of drinking water with the opening of the Washington Aqueduct in 1864 using a water intake constructed at Great Falls HydrologyWater supply and water quality An average of approximately 486 million US gallons 1 840 000 m3 of water is withdrawn daily from the Potomac in the Washington area for water supply providing about 78 percent of the region s total water usage this amount includes approximately 80 percent of the drinking water consumed by the region s estimated 6 1 million residents The Potomac River surges over the deck of Chain Bridge during the historic 1936 flood The bridge was so severely damaged by the raging water and the debris it carried that its superstructure had to be re built the new bridge was opened to traffic in 1939 This photograph was taken from a vantage point on Glebe Road in Arlington County Virginia The houses on the bluffs in the background are located on the Potomac Palisades of Washington DC As a result of damaging floods in 1936 and 1937 the Army Corps of Engineers proposed the Potomac River basin reservoir projects a series of dams that were intended to regulate the river and to provide a more reliable water supply One dam was to be built at Little Falls just north of Washington backing its pool up to Great Falls Just above Great Falls the much larger Seneca Dam was proposed whose reservoir would extend to Harpers Ferry Several other dams were proposed for the Potomac and its tributaries Dams on the Potomac River Operational Little Falls Dam Potomac River aka Brookmont Dam at C amp O Canal milepost 5 6 upstream of Chain Bridge Potomac Aqueduct Dam at C amp O Canal milepost 17 5 upstream of Great Falls C amp O Feeder Dam No 4 at C amp O Canal milepost 84 downstream of Williamsport MD Honeywood Dam aka C amp O Feeder Dam No 5 at C amp O Canal milepost 106 upstream of Williamsport MD Cumberland Dam aka Feeder Dam No 8 on North Branch of Potomac River 40 miles downstream of Fairfax Stone Jennings Randolph Dam on North Branch of the Potomac River 27 miles downstream of Fairfax Stone Non Operational C amp O Feeder Dam No 1 C amp O Canal milepost 5 6 upstream of Chain Bridge near Lock 6 associated with Little Falls Skirting Canal 1 Seneca Dam aka C amp O Feeder Dam No 2 at C amp O Canal milepost 22 near Violette s Lock Armory Dam aka C amp O Feeder Dam No 3 at C amp O Canal milepost 62 upstream of Harpers Ferry WV C amp O Feeder Dam No 6 Archived August 31 2020 at the Wayback Machine at C amp O Canal milepost 134 west of Hancock MD Planned but never built C amp O Feeder Dam No 7 and Guard Lock No 7 were proposed to be located near milepost 164 close to the mouth of the South Branch of the Potomac but were never built due to financial considerations When detailed studies were issued by the Corps in the 1950s they met sustained opposition led by U S Supreme Court Justice William O Douglas resulting in the plans abandonment The only dam project that did get built was Jennings Randolph Lake on the North Branch The Corps built a supplementary water intake for the Washington Aqueduct at Little Falls in 1959 In 1940 Congress passed a law authorizing the creation of an interstate compact to coordinate water quality management among states in the Potomac basin Maryland West Virginia Pennsylvania Virginia and the District of Columbia agreed to establish the Interstate Commission on the Potomac River Basin The compact was amended in 1970 to include coordination of water supply issues and land use issues related to water quality Eutrophication in the Potomac River is evident from this bright green water in Washington D C caused by a dense bloom of cyanobacteria April 2012 Beginning in the 19th century with increasing mining and agriculture upstream and urban sewage and runoff downstream the water quality of the Potomac River deteriorated This created conditions of severe eutrophication It is said that President Abraham Lincoln used to escape to the highlands on summer nights to escape the river s stench In the 1960s with dense green algal blooms covering the river s surface President Lyndon Johnson declared the river a national disgrace and set in motion a long term effort to reduce pollution from sewage and restore the beauty and ecology of this historic river One of the significant pollution control projects at the time was the expansion of the Blue Plains Advanced Wastewater Treatment Plant which serves Washington and several surrounding communities Enactment of the 1972 Clean Water Act led to construction or expansion of additional sewage treatment plants in the Potomac watershed Controls on phosphorus one of the principal contributors to eutrophication were implemented in the 1980s through sewage plant upgrades and restrictions on phosphorus in detergents By the end of the 20th century notable success had been achieved as massive algal blooms vanished and recreational fishing and boating rebounded Still the aquatic habitat of the Potomac River and its tributaries remain vulnerable to eutrophication heavy metals pesticides and other toxic chemicals over fishing alien species and pathogens associated with fecal coliform bacteria and shellfish diseases In 2005 two federal agencies the US Geological Survey and the Fish and Wildlife Service began to identify fish in the Potomac and tributaries that exhibited intersex characteristics as a result of endocrine disruption caused by some form of pollution On November 13 2007 the Potomac Conservancy an environmental group issued the river a grade of D plus citing high levels of pollution and the reports of intersex fish Since then the river has improved with a reduction in nutrient runoff return of fish populations and land protection along the river As a result the same group issued a grade of B for 2017 and 2018 In March 2019 the Potomac Riverkeeper Network launched a laboratory boat dubbed the Sea Dog which will be monitoring water quality in the Potomac and providing reports to the public on a weekly basis in that same month the catching near Fletcher s Boat House of a Striped Bass estimated to weigh 35 lb 16 kg was seen as a further indicator of the continuing improvement in the health of the river Top Ten Historic Crests of the Potomac River 1877 2017Kitzmiller Hancock Williamsport ShepherdstownHarpers Ferry Point of Rocks Little Falls GeorgetownSource National Weather ServiceDischarge This chart displays the Annual Mean Discharge of the Potomac River measured at Little Falls Maryland for Water Years 1931 2017 in cubic feet per second Source of data USGS The average daily flow during the water years 1931 2018 was 11 498 cubic feet 325 6 m3 s The highest average daily flow ever recorded on the Potomac at Little Falls Maryland near Washington D C was in March 1936 when it reached 426 000 cubic feet 12 100 m3 s The lowest average daily flow ever recorded at the same location was 601 0 cubic feet 17 02 m3 s in September 1966 The highest crest of the Potomac ever registered at Little Falls was 28 10 ft on March 19 1936 however the most damaging flood to affect Washington DC and its metropolitan area was that of October 1942 Legal issuesBoundary between Maryland Virginia and West Virginia at Harpers Ferry Satellite view of the Potomac River passing through two water gaps downstream of Harpers Ferry For 400 years Maryland and Virginia have disputed control of the Potomac and its North Branch since both states original colonial charters grant the entire river rather than half of it as is normally the case with boundary rivers In its first state constitution adopted in 1776 Virginia ceded its claim to the entire river but reserved free use of it an act disputed by Maryland Both states acceded to the 1785 Mount Vernon Compact and the 1877 Black Jenkins Award which granted Maryland the river bank to bank from the low water mark on the Virginia side while permitting Virginia full riparian rights short of obstructing navigation From 1957 to 1996 the Maryland Department of the Environment MDE routinely issued permits applied for by Virginia entities concerning the use of the Potomac However in 1996 the MDE denied a permit submitted by the Fairfax County Water Authority to build a water intake 725 feet 220 m offshore citing potential harm to Maryland s interests by an increase in Virginia sprawl caused by the project After years of failed appeals within the Maryland government s appeal processes in 2000 Virginia took the case to the Supreme Court of the United States which exercises original jurisdiction in cases between two states Maryland claimed Virginia lost its riparian rights by acquiescing to MDE s permit process for 63 years MDE began its permit process in 1933 A Special Master appointed by the Supreme Court to investigate recommended the case be settled in favor of Virginia citing the language in the 1785 Compact and the 1877 Award On December 9 2003 the Court agreed in a 7 2 decision Map of land use in the watershed The original charters are silent as to which branch from the upper Potomac serves as the boundary but this was settled by the 1785 Compact When West Virginia seceded from Virginia in 1863 the question of West Virginia s succession in title to the lands between the branches of the river was raised as well as title to the river itself Claims by Maryland to West Virginia land north of the South Branch all of Mineral and Grant Counties and parts of Hampshire Hardy Tucker and Pendleton Counties and by West Virginia to the Potomac s high water mark were rejected by the Supreme Court in two separate decisions in 1910 FaunaFish After an absence lasting many decades the American Shad has recently returned to the Potomac A variety of fish inhabit the Potomac including bass muskellunge pike walleye The northern snakehead an invasive species resembling the native bowfin lamprey and American eel was first seen in 2004 Many species of sunfish are also present in the Potomac and its headwaters Although rare bull sharks can be found After having been depressed for many decades the river s population of American shad is currently re bounding as a result of the ICPRB s successful American Shad Restoration Project that was begun in 1995 In addition to stocking the river with more than 22 million shad fry the Project supervised the construction of a fishway that was built to facilitate the passage of adults around the Little Falls Dam on the way to their traditional spawning grounds upstream Freshwater fish of the Potomac RiverBowfin Amiidae Bowfin Amia calvaCatfishes Ictaluridae White bullhead catfish Ameiurus catus Yellow bullhead catfish Ameiurus natalis Brown bullhead catfish Ameiurus nebulosus Channel catfish Ictalurus punctatus Tadpole madtom Noturus gyrinus Margined madtom Noturus insignis Blue catfish Ictalurus furcatus Flathead catfish Pylodictis olivaris Eels Anguillidae American eel Anguilla rostrataGars Lepisosteidae Longnose gar Lepisosteus osseusHerrings Clupeidae Blueback herring Alosa aestivalis Hickory shad Alosa mediocris Alewife Alosa pseudoharengus American shad Alosa sapidissima Gizzard shad Dorosoma cepedianum Threadfin shad Dorosoma petenenseKillifishes Fundulidae Banded killifish Fundulus diaphanus Mummichog killifish Fundulus heteroclitus Spotfin killifish Fundulus luciae Striped killifish Fundulus majalis Rainwater killifish Lucania parvaPupfish Cyprinodontidae Sheepshead minnow Cyprinodon variegatusLampreys Petromyzontidae Least brook lamprey Lampetra aepyptera American brook lamprey Lampetra appendix Sea lamprey Petromyzon marinusMinnows Cyprinidae Central stoneroller Campostoma anomalum Goldfish Carassius auratus Redside dace Clinostomus elongatus Rosyside dace Clinostomus funduloides Grass carp Ctenopharyngodon idella Satinfin shiner Cyprinella analostana Spotfin shiner Cyprinella spiloptera Common carp Cyprinus carpio Cutlips minnow Exoglossum maxillingua Eastern silvery minnow Hybognathus regius Striped shiner Luxilus chrysocephalus Common shiner Luxilus cornutus Allegheny pearl dace Margariscus margarita River chub Nocomis micropogon Golden shiner Notemigonus crysoleucas Comely shiner Notropis amoenus Emerald shiner Notropis atherinoides Bridle shiner Notropis bifrenatus Silverjaw minnow Notropis buccatus Ironcolor shiner Notropis chalybaeus Spottail shiner Notropis hudsonius Swallowtail shiner Notropis procne Rosyface shiner Notropis rubellus Bluntnose minnow Pimephales notatus Fathead minnow Pimephales promelas Eastern blacknose dace Rhinichthys atratulus Longnose dace Rhinichthys cataractae Creek chub Semotilus atromaculatus Fallfish Semotilus corporalis Bluehead chub Nocomis leptocephalus Mimic shiner Notropis volucellusMudminnows Umbridae Eastern mudminnow Umbra pygmaeaPerches Percidae Greenside darter Etheostoma blennioides Rainbow darter Etheostoma caeruleum Fantail darter Etheostoma flabellare Swamp darter Etheostoma fusiforme Johnny darter Etheostoma nigrum Tessellated darter Etheostoma olmstedi Glassy darter Etheostoma vitreum Banded darter Etheostoma zonale Yellow perch Perca flavescens Common logperch Percina caprodes Stripeback darter Percina notogramma Shield darter Percina peltata Walleye Sander vitreumPercopsids Percopsidae Trout perch Percopsis omiscomaycusPikes Esocidae Redfin pickerel Esox americanus Northern pike Esox lucius Muskellunge Esox masquinongy Chain pickerel Esox nigerPirate perch Aphredoderidae Pirate perch Aphredoderus sayanusPoeciliids Poeciliidae Eastern mosquitofish Gambusia holbrooki Guppy Poecilia reticulataPupfish Cyprinodontidae Sheepshead minnow Cyprinodon variegatusSculpins Cottidae Mottled sculpin Cottus bairdii Blue Ridge sculpin Cottus caeruleomentum Potomac sculpin Cottus girardiSilversides Atherinopsidae Inland silverside Menidia beryllinaSmelts Osmeridae Rainbow smelt Osmerus mordaxSnakeheads Channidae Northern snakehead Channa argus Sturgeons Acipenseridae Shortnose sturgeon Acipenser brevirostrum Atlantic sturgeon Acipenser oxyrhinchusSuckers Catostomidae Quillback Carpiodes cyprinus White sucker Catostomus commersoni Creek chubsucker Erimyzon oblongus Northern hogsucker Hypentelium nigricans Golden redhorse Moxostoma erythrurum Shorthead redhorse Moxostoma macrolepidotum Torrent sucker Thoburnia rhothoecaSunfishes Centrarchidae Mud sunfish Acantharcus pomotis Rock bass Amblopites rupestris Flier sunfish Centrarchus macropterus Blackbanded sunfish Enneacanthus chaetodon Bluespotted sunfish Enneacanthus gloriosus Banded sunfish Enneacanthus obesus Redbreast sunfish Lepomis auritus Green sunfish Lepomis cyanellus Pumpkinseed sunfish Lepomis gibbosus Warmouth sunfish Lepomis gulosus Bluegill sunfish Lepomis macrochirus Longear sunfish Lepomis megalotis Redear sunfish Lepomis microlophus Smallmouth bass Micropterus dolomieu Largemouth bass Micropterus salmoides White crappie Pomoxis annularis Black crappie Pomoxis nigromaculatusTemperate basses Moronidae White perch Morone americana Striped bass Morone saxatilisTrout and whitefish Salmonidae Rainbow trout Oncorhynchus mykiss Brown trout Salmo trutta denotes naturalized species Sources Dnr state md Fish key of native species http www potomacriver org wp content uploads 2014 11 MasterFreshFishList0213 pdfTidal freshwater fish of the Potomac RiverMullets Mugilidae Striped mullet Mugil cephalus Drums Sciaenidae Spot Leiostomus xanthurus Spotted seatrout Cynoscion nebulosus Atlantic Croaker Micropogonias undulatus Red drum Sciaenops ocellata Soles Soleidae Hogchoker Trinectes maculatus Sharks Carcharhinidae Bull shark Carcharhinus leucas Sources Dnr state md Fish key of native species http www potomacriver org wp content uploads 2014 11 MasterFreshFishList0213 pdfMammals Several hundred bottle nosed dolphins live six months of the year from mid April through mid October in the Potomac Depicted here a mother with her young Mammals of the Potomac River BasinBats Little brown bat Myotis lucifugus Indiana bat Myotis sodalis Eastern small footed bat Myotis leibii Northern long eared bat Myotis septentrionalis Silver haired bat Lasionycteris noctivagans Tricolored bat Perimyotis subflavus Big brown bat Eptesicus fuscus Red bat Lasiurus borealis Hoary bat Lasiurus cinereus Evening bat Nycticeius humeralis Bears American black bear Ursus americanus Beavers American beaver Castor canadensis Cats Bobcat Lynx rufus Cougar Puma concolor extirpated Eastern cougar P c couguar extinct Canids Red fox Vulpes vulpes Gray fox Urocyon cinereoargenteus Coyote Canis latrans Gray wolf Canis lupus extirpated Red wolf Canis rufus extirpated Ungulates Sika deer Cervus nippon Elk Cervus canadensis reintroduced Eastern elk C c canadensis extinct Rocky Mountain elk C c canadensis introduced White tailed deer Odocoileus virginianus American bison Bison bison extirpated Jumping mice Meadow jumping mouse Zapus hudsonius Woodland jumping mouse Napaeozapus insignis Lemmings Southern bog lemming Synaptomys cooperi Marine Mammals Bottlenose dolphin Tursiops truncatus Moles Hairy tailed mole Parascalops breweri Eastern mole Scalopus aquaticus Southeastern star nosed mole Condylura cristata parva Muskrats Muskrat Ondatra zibethicus New World Mice and Rats Marsh rice rat Oryzomys palustris Deer mouse Peromyscus maniculatus White footed deer mouse Peromyscus leucopus Allegheny woodrat Neotoma magister Nutria Nutria Myocastor coypus Old World mice and rats Black rat Rattus rattus Norway rat Rattus norvegicus House mouse Mus musculus Opossums Virginia opossum Didelphis virginiana Porcupines Porcupine Erethizon dorsatum Rabbits and Hares Eastern cottontail Sylvilagus floridanus Appalachian cottontail Sylvilagus obscurus Raccoons Raccoon Procyon lotor Shrews Masked shrew Sorex cinereus Southeastern shrew Sorex longirostris Southern water shrew Sorex palustris punctulatus Smoky shrew Sorex fumeus Long tailed shrew Sorex dispar Southern pygmy shrew Sorex hoyi winnemana Northern short tailed shrew Blarina brevicauda Least shrew Cryptotis parva Skunks Eastern spotted skunk Spilogale putorius Striped skunk Mephitis mephitis Squirrels and chipmunks Eastern chipmunk Tamias striatus Groundhog aka Woodchuck Marmota monax Eastern gray squirrel Sciurus carolinensis Eastern fox squirrel Sciurus niger Delmarva fox squirrel S n cinereus Red squirrel Tamiasciurus hudsonicus Southern flying squirrel Glaucomys volans Voles Southern red backed vole Clethrionomys gapperi Meadow vole Microtus pennsylvanicus Southern rock vole Microtus chrotorrhinus carolinensis Woodland vole Microtus pinetorum Mustelids Fisher Pekania pennanti Least weasel Mustela nivalis American ermine Mustela richardsonii Long tailed weasel Neogale frenata American mink Neogale vison Northern river otter Lontra canadensis denotes introduced species Sources Mammals of Maryland Maryland Department of Natural Resources Retrieved February 8 2018 Wildlife Information Virginia Department of Wildlife Resources Retrieved July 4 2020 Mammals of West Virginia A Field Checklist 2001 West Virginia Division of Natural Resources Wildlife Resources Section Retrieved February 8 2018 Early European colonists who settled along the Potomac found a diversity of large and small mammals living in the dense forests nearby Bison elk wolves both gray and red and cougars were still present at that time but had been hunted to extirpation by the middle of the 19th century Among the denizens of the Potomac s banks beavers and otters met a similar fate while small populations of American mink and American martens survived into the 20th century in some secluded areas There is no record of early settlers having observed marine mammals in the Potomac but several sightings of Atlantic bottle nosed dolphins Tursiops truncatus were reported during the 19th century In July 1844 a pod of 14 adults and young was followed up the river by men in boats as high as the Aqueduct Bridge approximately the same location occupied by Key Bridge today Since 2015 perhaps as a result of warmer temperatures rising water levels in the Chesapeake Bay and improving water quality in the Potomac unprecedented numbers of Atlantic bottle nosed dolphins have been observed in the river According to Dr Janet Mann of Georgetown University s Potomac Chesapeake Dolphin Project more than 500 individual members of the species have been identified in the Potomac during this period Birds Birds of the Potomac River BasinReptiles Eastern box turtles are frequently spotted along the towpath of the C amp O Canal Turtles of the Potomac River BasinBog Muhlenberg turtle Glyptemys Clemmys muhlenbergii Chinese softshell turtle Pelodiscus sinensis Coastal plain cooter Pseudemys concinna floridana Cumberland slider Trachemys scripta troostii Eastern box turtle Terrapene carolina carolina Eastern chicken turtle Deirochelys reticularia reticularia Eastern mud turtle Kinosternon subrubrum subrubrum Eastern musk turtle Sternotherus odoratus Eastern painted turtle Chrysemys picta picta Eastern river cooter Pseudemys concinna concinna Eastern spiny softshell turtle Apalone spinifera spinifera Green sea turtle Chelonia mydas Gulf Coast spiny softshell turtle Apalone spinifera aspera Hawksbill sea turtle Eretmochelys imbricata Kemp s ridley sea turtle Lepidochelys kempii Leatherback sea turtle Dermochelys coriacea Loggerhead sea turtle Caretta caretta Mississippi map turtle Graptemys pseudogeographica kohnii Northern map turtle Graptemys geographica Northern diamond backed terrapin Malaclemys terrapin terrapin Northern red bellied cooter Pseudemys rubriventris Red eared slider Trachemys scripta elegans Snapping turtle Chelydra serpentina Spotted turtle Clemmys guttata Striped mud turtle Kinosternon baurii Stripe necked musk turtle Sternotherus minor peltifer Wood turtle Glyptemys insculpta Yellow bellied slider Trachemys scripta scripta denotes naturalized species Sources https dwr virginia gov wp content uploads virginia native naturalized species pdf http dnr maryland gov wildlife Documents herpchecklist pdfSnakes of the Potomac River basinNorthern copperhead Agkistrodon contortrix mokasen Timber rattlesnake Crotalus horridus Northern watersnake Nerodia sipedon sipedon Nerodia erythrogaster erythrogaster Queen snake Regina septemvittata Eastern smooth earthsnake Virginia valeriae valeriae Mountain earthsnake Virginia valeriae pulchra Northern brown snake Storeria dekayi dekayi Northern Red bellied Snake Storeria occipitomaculata occipitomaculata Eastern garter snake Thamnophis sirtalis sirtalis Common ribbonsnake Thamnophis sauritus sauritus Southern ring necked snake Diadophis punctatus punctatus Northern ring necked snake Diadophis punctatus edwardsi Eastern worm snake Carphophis amoenus amoenus Smooth green snake Opheodrys vernalis Northern rough greensnake Opheodrys aestivus aestivus Eastern hog nosed snake Heterodon platirhinos Rainbow snake Farancia erytrogramma erytrogramma Northern Black Racer Coluber constrictor constrictor Red cornsnake Pantherophis guttatus Eastern ratsnake Pantherophis alleghaniensis Mole kingsnake Lampropeltis calligaster rhombomaculata Eastern kingsnake Lampropeltis getula getula Eastern kilksnake Lampropeltis triangulum triangulum Coastal Plain Milksnake Lampropeltis triangulum elapsoides Northern scarletsnake Cemophora coccinea copei Sources http dnr maryland gov wildlife Documents herpchecklist pdf A Guide to the Snakes of Virginia Virginia Department of Game and Inland Fisheries Wildlife Diversity Division Special Publication No 2 1 2002 by Michael J Pinder Author Five lined skink juvenileLizards of the Potomac River BasinEastern Fence Lizard Sceloporus undulatus Eastern Six lined Racerunner Aspidoscelis sexlineata sexlineata Little Brown Skink Scincella lateralis Northern Coal Skink Plestiodon anthracinus anthracinus Common Five lined Skink Plestiodon fasciatus Broad headed Skink Plestiodon laticeps Sources https dwr virginia gov wp content uploads virginia native naturalized species pdf http dnr maryland gov wildlife Documents herpchecklist pdfAmphibians Salamanders of the Potomac River BasinCommon Mudpuppy Necturus maculosus maculosus Eastern Hellbender Cryptobranchus alleganiensis alleganiensis Marbled Salamander Ambystoma opacum Jefferson Salamander Ambystoma jeffersonianum Spotted Salamander Ambystoma maculatum Eastern Tiger Salamander Ambystoma tigrinum tigrinum Red spotted Newt Notophthalmus viridescens viridescens Eastern Red backed Salamander Plethodon cinereus Wehrle s Salamander Plethodon wehrlei Northern slimy salamander Plethodon glutinosus Valley and ridge salamander Plethodon hoffmani Seal Salamander Desmognathus monticola monticola Northern Dusky Salamander Desmognathus fuscus Allegheny Mountain Dusky Salamander Desmognathus ochrophaeus Northern Red Salamander Pseudotriton ruber ruber Eastern Mud Salamander Pseudotriton montanus montanus Northern Spring Salamander Gyrinophilus porphyriticus porphyriticus Northern Two lined Salamander Eurycea bislineata Southern Two lined Salamander Eurycea cirrigera Long tailed salamander Eurycea longicauda longicauda Four toed Salamander Hemidactylium scutatum Green Salamander Aneides aeneus Sources https dwr virginia gov wp content uploads virginia native naturalized species pdf http dnr maryland gov wildlife Documents herpchecklist pdfFrogs and toads of the Potomac River BasinUpland Chorus Frog Pseudacris feriarum New Jersey Chorus Frog Pseudacris kalmi Northern Spring Peeper Pseudacris crucifer Mountain Chorus Frog Pseudacris brachyphona Eastern Cricket Frog Acris crepitans crepitans Green Treefrog Hyla cinerea Gray Treefrog Hyla versicolor Cope s Gray Treefrog Hyla chrysoscelis Barking Treefrog Hyla gratiosa Carpenter Frog Lithobates virgatipes Wood Frog Lithobates sylvaticus Northern Leopard Frog Lithobates pipiens Southern Leopard Frog Lithobates sphenocephalus utricularius Pickerel Frog Lithobates palustris Northern Green Frog Lithobates clamitans melanota American Bullfrog Lithobates catesbeiana Eastern spadefoot toad Scaphiopus holbrookii Eastern American Toad Anaxyrus americanus americanus Fowler s Toad Anaxyrus fowleri Eastern Narrow mouthed Toad Gastrophryne carolinensis denotes naturalized species Sources https dwr virginia gov wp content uploads virginia native naturalized species pdf http dnr maryland gov wildlife Documents herpchecklist pdfAdditional imagesUpper and lower Potomac The South Branch near South Branch Depot West Virginia Confluence of the Cacapon River barely visible with the Potomac Oblique air photo facing southwest of the Potomac River flowing through water gaps in the Blue Ridge Mountains Virginia on the left Maryland on the right West Virginia in upper right including Harpers Ferry partially obscured by Maryland Heights of Elk Ridge Mountain at the confluence of the Potomac and Shenandoah Rivers Potomac River at Goose Creek The Great Falls of the Potomac viewed from the Virginia bank of the river Engraving based on an aquatint drawn by George Jacob Beck in 1802 Tidal Potomac Potomac near Occoquan Bay View of the Potomac River Analostan Island Georgetown and in the distance buildings of the nascent City of Washington Engraving based on an 1801 watercolor by George Jacob Beck Jefferson Memorial in Washington D C viewed from across the Tidal Basin of the Potomac The Pentagon looking northeast with the Potomac in the distance img