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As the Nation's principal conservation agency, the Department of the Interior has responsibility for most of our nationally owned Basins of the public lands and natural resources. This includes fostering the : wisest use of our land and water resources, protecting our fish and wildlife, preserving the environmental and cultural values of our national parks and historical places, and providing for the enjoy­ The Potomac ment of life through outdoor recreation. The Department assesses our energy and mineral resources and works to assure that their development is in the best interests of all our people. The Depart­ ment also has a major responsibility for American Indian reservation communities and for people who live in Island Territories under U.S. administration.

U.S. Department of the Interior/Geological Survey River Basins of the United States: The Potomac

This leaflet, one of a series on the river basins of the United States, contains information on the Basin, including a brief early history, a description of the physical characteristics, and other statistical data. At present, other river basins included in the series are The Colorado, The Columbia, The , The Hudson, and The Wabash.

Early Exploration and Settlement Major Length The Potomac was discovered in 1608 by The South Branch of the Potomac River, The Potomac River is approximately 400 Captain who called the river the Savage, , Monocacy, and miles long from its headwaters at North "Patawomeke" after an Algonquian Indian Cacapon ; and Antietam and Branch to its mouth in the family place name for the area that is now Conococheague Creeks are major tribu­ . It ranks 48th among 135 U.S. rivers that Washington, D.C. The basin area was first taries of the Potomac. are more than 100 miles long. inhabited by three Indian tribes of the Algonquian family group and Course Width in what is now and The North and South Branches flow The river is about 11 miles wide be­ Nanticoke in what is now . The northeast and unite about 15 miles southeast tween Point Lookout and Smith Point. first settlement of Europeans was established of Cumberland, Md. The river then flows Upstream, from Great Falls to Harpers Fer­ in 1634 in the Colony of Maryland by the east-southeast, with frequent meanders, ry, it averages about 1,300 feet in width. second Lord , Cecil Calvert. forming the Maryland- and Maryland-Virginia boundaries. Passing Depth Headwaters Harpers Ferry, W. Va., it flows through a relatively steep-sided valley, interrupted by The deepest point near Morgantown, Md., The North Branch of the Potomac River in the tidal portion of the river below Wash­ (mainstream headwater) rises in the western intermittent and riffles. Ten miles ington, D.C., is 107 feet. A navigable near Fairfax Stone, a north of Washington, the river has cut a channel depth of 24 feet is maintained for monument at the Maryland-West Virginia 200-foot gorge in which it descends some 108 miles in the tidal portion of the river, boundary. 90 feet in a 3-mile series of rapids known as the Great Falls of the Potomac. Below downstream from Washington, D.C. Great Falls and past Washington to Mount Mouth Vernon, the river flows at moderate depths Rate of Flow The Potomac enters along gently sloping banks. At Washington, Near the headwaters at Cumberland, Md., between Point Lookout, Md., and Smith still 116 miles from its mouth, it meets the the river's rate of flow is 559,000 gallons Point, Va. The approximate latitude at the and becomes an . The Potomac per minute (gpm); about midpoint at Point mouth is 38°00' N. and the approximate longi­ enters the Chesapeake Bay about 73 miles of Rocks, Md., it is 4.2 million gpm; and the tude is 76°15' W. from the Atlantic . rate of flow at the start of the estuary near Washington, D.C., is 5.1 million gpm. Potomac River Basin Highest and Lowest Flows Average Rainfall ton; and limited hydroelectric power The highest recorded flow, about 216 An average of from 35 to 45 inches of generation are some of the ways in which million gpm, occurred at Washington, D.C., rain falls annually in most of the basin, water from the basin is used commercially. in March 1936; the lowest flow, 270,000 and more than 60 inches of rain fall at the gpm, occurred at Washington in September higher elevations of the basin. 1966. Agricultural products which come from Quality the basin are: fruit, grain, tobacco, forage Dams, , and From its headwaters to Washington, the wa­ crops, and dairy products. The Dam and is ter in the river is fresh; however, in the near Bloomington, Md., and the Stony River estuary below Washington, the water be­ Industry Dam and Reservoir is near Mount Storm, comes brackish. The river delivers 2Vz Industry in the basin includes: wood W. Va. The Chesapeake and million tons of sediment to the estuary in an pulp and textile mills, electronic and parallels the river from Cumberland, Md., average year. The water of the Potomac chemical industries, and a variety of light to Washington, D.C. The canal formerly was is usually hard (contains 121 to 180 parts industries. used for shipping, but with its towpath, it per million of undissolved solids per liter) is now a recreational area. and requires treatment. It is of good quality except for localized pollution from indus­ Minerals Geologic Setting trial wastes (including acid mine drainage), Minerals found in the basin are: limestone, municipal wastes, and sediment. Ground sand and gravel, glass sand, coal, shale, The Potomac River Basin lies in five physi­ water, where available, can be used with­ lead, zinc, soapstone, marble, pyrite, and ographic provinces: , Pied­ out treatment. manganese; and brick, fire, and ceramic clays. mont Plateau, , Valley and Ridge, and . The Valley and Ridge province includes the Shenandoah Major Cities Water Data Valley. The land is hilly to mountainous Chambersburg, Waynesboro, and Gettys­ The Hydrologic Data Network, maintained with frequent rock outcroppings in the up­ burg, Pa.; Silver Spring, Bethesda, Rockville, by the U.S. Geological Survey in coopera­ per area. From Harpers Ferry to the area Hagerstown, and Frederick, Md.; Arlington, tion with the individual States, is the chief above Washington, D.C., the land is open Alexandria, and Staunton, Va.; Martinsburg, source of basic data on water in this country. plain with scattered forest cover. West of Keyser, and Romney, W. Va.; and Wash­ In cooperation with other agencies, the the Blue Ridge province, rocks are folded ington, D.C., are major cities of the U.S. Geological Survey maintains sedimentary types including limestone, dolo­ Potomac River Basin. 16,500 gaging stations that measure high mite, sandstone, and shale. From the Blue and low flow of rivers, lakes, and streams; Ridge province to Washington, rocks are Municipal and Industrial Water Use 27,500 observation wells that collect data on metamorphic (mainly crystalline) and levels and pumpage of ground water; and igneous types. From Washington to the About 2 1/2 million people use approxi­ 8,200 stations that measure . mouth of the river, sedimentary rocks and mately 450 million gallons of river water each alluvium predominate. day. About Vz million people on farms, in small towns, and in suburbs use about This publication is one of a series of general interest 100 million gallons of ground water each day. publications prepared by the U.S. Geological Survey to provide Drainage Area information about the sciences, natural resources, and the environment. To obtain a catalog of additional titles in the The basin area is 14,670 square miles and Commercial Water Use series "General Interest Publications of the U.S. Geological includes the District of Columbia and parts Survey," write: of Maryland, , Virginia, and Shipping from Washington to the Book and Open-File Reports Section Chesapeake Bay; fishing in the estuary; U.S. Geological Survey West Virginia. Federal Center, Box 25425 recreation and resort areas above Washing­ Denver, CO 80225

. GOVERNMENT PRINTING OFFICE: 1988-211-19?