Potomac River

The Potomac River (/pəˈtoʊmək/ (listen)) 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,^[4] with a drainage area of 14,700 square miles (38,000 km²),^[5] 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.

Potomac River
Great Falls of the Potomac River in June 2017 ^[1]
The Potomac River watershed covers the District of Columbia and parts of four states
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 / 39.19528; -79.49111
• elevation	3,060 ft (930 m)
2nd source	South Branch
• location	Near Monterey, Highland County, Virginia
• coordinates	38°25′30″N 79°36′30″W / 38.4251202°N 79.6083824°W / 38.4251202; -79.6083824
Source confluence
• location	Green Spring, West Virginia
• coordinates	39°31′42″N 78°35′16″W / 39.52833°N 78.58778°W / 39.52833; -78.58778
Mouth	Chesapeake Bay
• location	St. Mary's County, Maryland/Northumberland County, Virginia, United States
• coordinates	37°59′54″N 76°20′02″W / 37.9982645°N 76.3338878°W / 37.9982645; -76.3338878
• elevation	0 ft (0 m)
Length	405 mi (652 km)
Basin size	14,700 sq mi (38,000 km^2)
Discharge
• location	Little Falls, near Washington, D.C. (non-tidal; water years: 1931–2018)^[2]
• average	11,498 cu ft/s (325.6 m^3/s) (1931–2018)
• minimum	4,017 cu ft/s (113.7 m^3/s) (2002)
• maximum	23,760 cu ft/s (673 m^3/s) (1996)
Discharge
• location	Point of Rocks, Maryland
• average	9,504 cu ft/s (269.1 m^3/s)
Discharge
• location	Hancock, Maryland
• average	4,168 cu ft/s (118.0 m^3/s)
Discharge
• location	Paw Paw, West Virginia
• average	3,376 cu ft/s (95.6 m^3/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^[3]

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.

Course

 

The 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 miles (652 km) from Fairfax Stone Historical Monument State Park in West Virginia on the Allegheny Plateau to Point Lookout, Maryland, and drains 14,679 square miles (38,020 km²). The length of the river from the junction of its North and South Branches to Point Lookout is 302 miles (486 km).^[4]

 

Map showing the five geological provinces through which the Potomac River flows ^[6]

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.

v t e Route map of the Potomac River from the confluence of its North and South Branches to the Chesapeake Bay
Legend
North Branch Potomac River West Virginia Maryland     South Branch Potomac River   Town Creek   Little Cacapon River   Fifteenmile Creek   Paw Paw Bridge;    WV 9 / MD 51   Sideling Hill Creek   Cacapon River   Sir Johns Run   Grasshopper Run   Hancock Bridge;   US 522   Warm Spring Run   Tonoloway Creek   Sleepy Creek   Licking Creek   Cherry Run   Back Creek   Little Conococheague Creek   Conococheague Creek   Williamsport Pike Bridge;   US 11   Maryland Veterans Memorial Bridge;   I-81   Opequon Creek   Rumsey (Shepherdstown) Bridge;    WV 480 / MD 34   Rattlesnake Run   Packhouse Ford   Antietam Creek     ″The Needles″ Rapids   Shenandoah River       Potomac Water Gap between Blue Ridge Mt (VA/WV) and Elk Ridge Mt (MD)   Harpers Ferry Whitewater Pool     White Horse Rapids       West Virginia Virginia       Potomac Water Gap between Short Hill Mt (VA) and South Mt (MD)   Sandy Hook Bridge;   US 340   Israel Creek   Brunswick Bridge;    SR 287 / MD 17   Catoctin Creek   Little Catoctin Creek   Catoctin Creek       Potomac Water Gap between Furnace Mt (VA) and Pine Rock (MD)   Point of Rocks Bridge;   US 15   Heaters Island WMA (MD)   White's Ford   Nolands Ferry (historic)   Tuscarora Creek   Cheek's Ford   Monocacy River   Little Monocacy River   Mason Island WMA (MD)       White's Ferry;    SR 655 / MD 107     Ball's Bluff (VA) and Harrison Island (MD)   Broad Run   Edwards Ferry (historic)   Goose Creek   Selden Island (MD)   Broad Run   Horsepen Creek   Horsepen Branch     McKee-Beshers Wildlife MGT Area   Sharpshin Island (MD)   Sugarland Run   Old Sugarland Run   Rowsers Ford     Seneca Redstone Quarry (historic)   Seneca Creek     Seneca Rapids     Blockhouse Point Promontory   Muddy Branch   Nichols Run   Watts Branch   Gladys Island (Potomac River) (MD)   Cool Spring Branch   Conn's Ferry (historic)   Conn Island (Potomac River) (MD)   Limekiln Branch       Aqueduct Dam (supplies water to the Washington Aqueduct) ^[AQU]     Beginning of Potomac Gorge   Great Falls   Carroll Branch     O-Deck Rapids   Olmsted Island (formerly Great Falls Island) (MD)     Glade Hill (boulders and sediment left by the ancestral Potomac River)^[GHL]   Mine Run Branch     Fishladder Rapids   Bear Island and Billy Goat Trail, Section A (Maryland)   Sherwin Island (formerly Cupid's Bower Island) (MD)     S-Turn Rapids     Rocky Island Rapids   Rocky Island(s) and Hidden Gorge (MD)     Ruins of Matildaville     Beginning of Mather Gorge     Wet Bottom Rapids     Sandy Landing (boat ramp; take-out only)   Difficult Run     Difficult Run Rapids     Cow Hoof Rock and Black Pond (site of most recent paleo-falls >30 kya) ^[BLK] (VA)   Offutt Island (MD)     Offutt Island Rapids   Bullneck Run   Rock Run   Turkey Island (MD)     Calico Rapids-Yellow Rapids   Scott's Run     Scott's Run Nature Preserve     Stubblefield Rapids and Knickpoint (paleo falls ~200 kya)     End of Mather Gorge   American Legion/Cabin John Bridge;   I-495 Capital Beltway   Plummers Island (MD)         Plummers Island Thrust Fault (inactive) ^[PIF]   Dead Run     Dead Run Rapids   Turkey Run (Potomac River)   Cabin John Creek   Minnehaha Branch   Sycamore Island (MD)       Little Falls Dam and Dalecarlia Reservoir   High Island   Little Falls   Little Falls Branch       Maryland District of Columbia     Western boundary of the Atlantic Seaboard fall line; Potomac Estuary begins ^[PES]   Chain Bridge;   SR 123 and Canal Road + Clara Barton Pkwy   Pimmit Run   Gulf Branch   Donaldson Run   Windy Run   Spout Run   Maddox Branch   Three Sisters Island   Foundry Branch   Ruins of Aqueduct Bridge   Francis Scott Key Bridge;   US 29   Rock Creek     End of Potomac Gorge   Limit of navigation; Eastern boundary of the Atlantic Seaboard fall line   Theodore Roosevelt Island^[TRI] (DC)   Theodore Roosevelt Bridge;    I-66 / US 50   Rocky Run (paved over)   Columbia Island (DC)   Arlington Memorial Bridge   Tidal Basin and Washington Channel   George Mason Memorial Bridge;    I-395 south / US 1 south   Rochambeau Memorial Bridge;    I-395 HOV  / US 1   Arland D. Williams Jr. Memorial Bridge;    I-395 north / US 1 north     Roaches Run Waterfowl Sanctuary   Tiber Creek (paved over)     Hains Point   Anacostia River   Four Mile Run   Oxon Creek       District of Columbia Maryland   Woodrow Wilson Bridge;    I-95 / I-495 Capital Beltway   Jones Point Light   Hunting Creek     Dyke Marsh Wildlife Preserve   Broad Creek   Henson Creek   Swan Creek   Piscataway Creek   Little Hunting Creek     Mount Vernon Estate   Dogue Creek   Accotink Creek   Pohick Creek   Pomonkey Creek     Mason Neck Wildlife Refuge   Occoquan River     Featherstone National Wildlife Refuge   Neabsco Creek   Powells Creek   Mattawoman Creek   Chicamuxen Creek   Quantico Creek   Chopawamsic Island (VA)   Chopawamsic Creek   Tank Creek   Aquia Creek     Crow's Nest Natural Area Preserve   Potomac Creek   Nanjemoy Creek   Chotank Creek   Port Tobacco River   Popes Creek   Gambo Creek   Clifton Creek   Governor Harry W. Nice Memorial Bridge;   US 301   Piccowaxen Creek   Upper Machodoc Creek   Wicomico River   Cobb Island (MD)   St. Clement's Island (MD)   Monroe Creek   Mattox Creek   Popes Creek   St. Marys River   Yeocomico River   Coan River   Hull Creek   Point Lookout Light   Smith Point Light   Debouchment of the Potomac Estuary       Chesapeake Bay

North Branch Potomac River

Main article: 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 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,^[4] 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

Main article: South Branch Potomac River

The exact location of 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 parallelsthe river until its mouth at Green Spring.

 

Canoers 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 South Branch River Road (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.^[7] 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, Catoctin Creek, 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.^[8] 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, Broad 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, Chicamuxen Creek, Quantico Creek, Little Creek, Chopawamsic Creek, Tank Creek, Aquia Creek, Potomac Creek, Nanjemoy Creek, Chotank Creek, Port Tobacco River, Popes Creek, Gambo Creek, Clifton Creek, Piccowaxen Creek, Upper Machodoc Creek, Wicomico River, Cobb Island, Monroe Creek, Mattox Creek, Popes Creek, Breton Bay, Leonardtown, St. Marys River, Yeocomico River, Coan River, and Hull Creek.

History

Natural history

The river itself is at least 3.5 million years old,^[6] 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.^[9]

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.^[10] Native Americans had different names for different parts of the river, calling the river above Great Falls Cohongarooton, meaning "honking geese"^[11][12] and "Patawomke" below the Falls, meaning "river of swans".^[13] 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".^[12] The river's name was officially decided upon as "Potomac" by the Board on Geographic Names in 1931.^[14]

 

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.^[15]

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.^[16][17][18]

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, Virginia

 

The Potomac running next to the Lincoln Memorial and under the Arlington Memorial Bridge.

Civil War Era

 

Confederate 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 Ferry

 

Union soldiers manning the Lower Battery at the north end of Chain Bridge in 1862.

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 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 circa 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.^[19] 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.^[20] 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.

See also: Attempts to make the Potomac River navigable

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.^[21][22]

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.^[5][23]

 

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,^[24] 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.^[25] 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&O Canal milepost 5.6, upstream of Chain Bridge) Potomac Aqueduct Dam (at C&O Canal milepost 17.5, upstream of Great Falls) C&O Feeder Dam No. 4 (at C&O Canal milepost 84, downstream of Williamsport, MD) Honeywood Dam aka C&O Feeder Dam No. 5 (at C&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&O Feeder Dam No. 1 (C&O Canal milepost 5.6, upstream of Chain Bridge near Lock 6; associated with Little Falls Skirting Canal [1] ) Seneca Dam aka C&O Feeder Dam No. 2 (at C&O Canal milepost 22, near Violette's Lock) Armory Dam aka C&O Feeder Dam No. 3 (at C&O Canal milepost 62, upstream of Harpers Ferry, WV)^[26] C&O Feeder Dam No. 6 August 31, 2020, at the Wayback Machine (at C&O Canal milepost 134, west of Hancock, MD)^[27] Planned, but never built C&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.^[28]

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.^[29] The only dam project that did get built was Jennings Randolph Lake on the North Branch.^[30] The Corps built a supplementary water intake for the Washington Aqueduct at Little Falls in 1959.^[31]

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.^[32]

 

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.^[33] 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.^[32]

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.^[34]

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.^[35] 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.^[36] 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;^[37] in that same month, the catching near Fletcher's Boat House of a Striped Bass estimated to weigh 35 lbs was seen as a further indicator of the continuing improvement in the health of the river.^[38]

Top Ten Historic Crests of the Potomac River, 1877–2017
Kitzmiller	Hancock	Williamsport	Shepherdstown
Harpers Ferry	Point of Rocks	Little Falls	Georgetown
Source: National Weather Service

Discharge

 

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^[2]

The average daily flow during the water years 1931–2018 was 11,498 cubic feet (325.6 m³) /s.^[2] 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.^[2] The lowest average daily flow ever recorded at the same location was 601.0 cubic feet (17.02 m³) /s in September 1966^[2] The highest crest of the Potomac ever registered at Little Falls was 28.10 ft, on March 19, 1936;^[39][24] however, the most damaging flood to affect Washington, DC and its metropolitan area was that of October 1942.^[40]

Legal issues

 

Boundary 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.^[41]

 

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.^[42][43]

Flora and fauna

Fish

 

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.^[44][45] Many types of sunfish are also present in the Potomac and its headwaters.^[46] Although rare, bull sharks can be found.^[47]

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.^[48]

Freshwater fish of the Potomac River

Bowfin (Amiidae) Bowfin Amia calva Catfishes (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 rostrata Gars (Lepisosteidae) Longnose gar Lepisosteus osseus Herrings (Clupeidae) Blueback herring Alosa aestivalis Hickory shad Alosa mediocris Alewife Alosa pseudoharengus American shad Alosa sapidissima Gizzard shad Dorosoma cepedianum Threadfin shad Dorosoma petenense Killifishes (Fundulidae) Banded killifish Fundulus diaphanus Mummichog killifish Fundulus heteroclitus Spotfin killifish Fundulus luciae Striped killifish Fundulus majalis Rainwater killifish Lucania parva Pupfish (Cyprinodontidae) Sheepshead minnow Cyprinodon variegatus Lampreys (Petromyzontidae) Least brook lamprey Lampetra aepyptera American brook lamprey Lampetra appendix Sea lamprey Petromyzon marinus Minnows (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 volucellus Mudminnows (Umbridae) Eastern mudminnow Umbra pygmaea Perches (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 vitreum Percopsids (Percopsidae) Trout-perch Percopsis omiscomaycus Pikes (Esocidae) Redfin pickerel Esox americanus Northern pike Esox lucius Muskellunge Esox masquinongy Chain pickerel Esox niger Pirate perch (Aphredoderidae) Pirate perch Aphredoderus sayanus Poeciliids (Poeciliidae) Eastern mosquitofish Gambusia holbrooki Guppy Poecilia reticulata Pupfish (Cyprinodontidae) Sheepshead minnow Cyprinodon variegatus Sculpins (Cottidae) Mottled sculpin Cottus bairdii Blue Ridge sculpin Cottus caeruleomentum Potomac sculpin Cottus girardi Silversides (Atherinopsidae) Inland silverside Menidia beryllina Smelts (Osmeridae) Rainbow smelt Osmerus mordax Snakeheads (Channidae) Northern snakehead* Channa argus* Sturgeons (Acipenseridae) Shortnose sturgeon Acipenser brevirostrum Atlantic sturgeon Acipenser oxyrhinchus Suckers (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 rhothoeca Sunfishes (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 nigromaculatus Temperate basses (Moronidae) White perch Morone americana Striped bass Morone saxatilis Trout and whitefish (Salmonidae) Rainbow trout (Oncorhynchus mykiss) Brown trout (Salmo trutta)   * denotes naturalized species; Sources: http://www.potomacriver.org/wp-content/uploads/2014/11/MasterFreshFishList0213.pdf

Tidal freshwater fish of the Potomac River
Mullets (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: http://www.potomacriver.org/wp-content/uploads/2014/11/MasterFreshFishList0213.pdf

Mammals

 

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 Basin

Bats 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).^[49]

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.^[50]

Birds

Birds of the Potomac River Basin

Reptiles

 

Eastern box turtles are frequently spotted along the towpath of the C&O Canal.

Turtles of the Potomac River Basin

Bog (=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.pdf

Snakes of the Potomac River basin

Northern copperhead Agkistrodon contortrix mokasen Timber rattlesnake Crotalus horridus Northern watersnake Nerodia sipedon sipedon Red-bellied watersnake 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, juvenile

Lizards of the Potomac River Basin

Eastern 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.pdf

Amphibians

Salamanders of the Potomac River Basin

Common 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.pdf

Frogs and toads of the Potomac River Basin

Upland 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.pdf

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 Occonquan 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   East Branch of the Potomac (now called the Anacostia River) near its confluence with the mainstem Potomac in Washington. (Watercolor drawn in 1839 by Augustus Kollner)   View of the Potomac from Mount Vernon   Potomac River seen while landing at Reagan National Airport

Other   View northeast down the North Branch Potomac River from the Gorman-Gormania Bridge (U.S. Route 50) between Gormania, Grant County, West Virginia and Gorman, Garrett County, Maryland   The North Branch Potomac River near Piedmont, WV   The South Branch Potomac River near South Branch Depot, WV   The South Branch of the Potomac River at Millesons Mill, WV   Potomac River Watershed in West Virginia, Virginia, Pennsylvania, and Maryland

See also

• Air Florida Flight 90
• List of cities and towns along the Potomac River
• List of crossings of the Potomac River
• List of islands on the Potomac River
• List of rivers of Maryland
• List of rivers of Virginia
• List of rivers of West Virginia
• List of tributaries of the Potomac River
• List of variant names of the Potomac River
• Potomac Heritage Trail

Notes and references

Notes

• ^ AQU: The diversion dam at Great Falls, often called the "Aqueduct Dam", was built in the 1850s by the US Army Corps of Engineers as part of the project assigned to them by Congress to supply clean water from above Great Falls to Washington, DC. Water diverted by the dam flows 12 miles through a 9-foot diameter pipeline to Dalecarlia Reservoir on the outskirts of the city where it is first allowed to settle and then filtered and purified before being distributed to consumers. Since 1927, potable water from Dalecarlia has also been provided to Arlington County and some other sections of nearby northern Virginia through three 20-inch diameter pipelines that cross the Potomac under the deck of Chain Bridge. In addition, there is nearby a 4-foot diameter conduit constructed in 1967 that traverses the Potomac beneath the riverbed which is used primarily for backup purposes.^[51][52]
  
• ^ GHL: "Evidence of the ancient Potomac River bed can be seen in well-rounded boulders, smoothed surfaces and grooves, and beautifully formed potholes. Look for sandstone boulders along the trail, which were deposited by massive floods. The sandy soils along the river trail, with shells mixed in, are a result of sediment deposits from floods. Some of the oldest sediment deposits in the area can be found on Glade Hill, between the Matildaville and Carriage Road trails. Glade Hill was once an island in the Potomac River, and the deposits found there were left before Mather Gorge formed."^[53]
  
• ^ PIF: "In the Late Pennsylvanian, the rocks of the Stubblefield Falls domain of the Mather Gorge Formation moved up relative to the Sykesville Formation on the steep, west-dipping Plummers Island fault and mylonite zones (Schoenborn, 2001) within an existing Plummers Island shear zone (figs. 5, 6). Shearing formed S2 cleavage with below-closure muscovite growth and more pervasive S2 cleavage in the Sykesville Formation. By the earliest Permian, all of the rocks in the Potomac terrane had cooled through 235°C (figs. 3, 5). Apatite fission-track data indicate cooling through ~90°C to 100°C in Early Jurassic to Early Cretaceous time, with increasing ages to the east, suggesting kilometer-scale rotation of the Potomac terrane in the Cretaceous and (or) Tertiary, with the west side up."^[54]
  
• ^ BLK: "Two samples collected from the terrace dissected by Great Falls indicate that the Falls were established in their current location by 30 ky. A series of 6 samples taken from a vertical transect just below the falls, indicates that vertical incision continued a rate of 0.5 m/ky between 27 and 12 ky, increasing to nearly 1.0 m/ky during the Holocene. These data suggest that the drop over Great Falls is growing with time. A dramatic increase in outcrop weathering and soil depth 3.5 km downstream of the Falls, suggests that prior to establishment of the Great Falls knickzone, a similar feature was likely present near Black Pond. 10-Be data are not yet available for this paleo knick zone; however, a 10-Be model age >200 ky from the top of Plummers island 5 km down stream of Black Pond suggests a much older period of retreat led to the formation of the Black Pond paleo knick zone."^[55]
  
• ^ PES: "The Potomac Estuary: From the Chain Bridge in Washington, DC, to Point Lookout at the confluence with the Chesapeake Bay, the Potomac Estuary is a long and narrow estuary—approximately 189 km. With its many tributaries and bays, however, the Potomac Estuary has a shoreline of 1,800 km. The Estuary meanders in a south, southeasterly direction, except for a sharp bend about halfway downriver. The Estuary has three well-defined and distinct zones. The upper zone, from Chain Bridge to Indian Head, is the tidal freshwater reach, with salinities of less than 0.5 parts per thousand (ppt). The middle reach, between Indian Head and the Route 301 Bridge at Morgantown, is the transition zone. The salinity of this zone varies from 0.5 to 7.0 ppt and is often referred to as the zone of maximum turbidity. The lower zone, from the 301 Bridge to Point Lookout, has salinities ranging from 7 to 16 ppt."^[56]
  
• ^ TRI: The rocky western (upriver) and central portions of the island are part of the Piedmont Plateau, while the southeastern part is within the Atlantic Coastal Plain. At one point opposite Georgetown, the Atlantic Seaboard fall line between the Piedmont and the Coastal Plain can be seen as a natural phenomenon. The island has about 2.5-mile (4.0 km) of shoreline, and the highest area of the island (where the Mason mansion stood) is about 44 feet (13 m) above sea level.
  

References

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Works cited

• Rice, James D., Nature and History in the Potomac Country: From Hunter-Gatherers to the Age of Jefferson. (2009), Baltimore: Johns Hopkins University Press; ISBN 0-8018-9032-2; ISBN 978-0-8018-9032-1
• Smith, J. Lawrence, The Potomac Naturalist: The Natural History of the Headwaters of the Historic Potomac (1968), Parsons, WV: McClain Printing Co.; ISBN 0-87012-023-9; ISBN 978-0-87012-023-7

External links