Rock Creek, Washington, D.C.
|County||Montgomery County, Maryland|
|Main source||Laytonsville, Maryland
560 feet (170 m)
|River mouth||Potomac River
0 feet (0 m)
|Length||32.6 miles (52.5 km)|
|Basin size||76.5 square miles (198 km2)|
|Landmarks||Rock Creek Park|
Rock Creek is a free-flowing tributary of the Potomac River, which empties into the Atlantic Ocean via the Chesapeake Bay. The creek is 32.6 miles (52.5 km) long, with a drainage area of about 76.5 square miles (198 km2). The last quarter-mile (400 m) of the creek is affected by tides.
The creek rises from a spring near Laytonsville in Montgomery County, in the U.S. state of Maryland, and joins the Potomac near Georgetown and the Watergate in Washington, D.C. Beginning in the Derwood-Rockville area in Maryland, the creek flows through Rock Creek Regional Park southward to the D.C. boundary. About 9 miles (14 km) of the creek flow though Rock Creek Park in Washington, where it is fed by several small creeks -- Piney Branch, Pinehurst Branch, Broad Branch, Soapstone Branch, and Luzon Branch -- and numerous storm sewers.
The Chesapeake and Ohio Canal joins Rock Creek in Georgetown, and used the mouth of Rock Creek as its terminus in Georgetown. At the Tidewater Lock, the creek (and the canal) empty into the Potomac River. This area, called the "Rock Creek Basin" by the Canal Company, which included a mole, causeway, and waste weir, was completed in 1831.:251 Subject to silting up, it was dredged several times for the Canal's use.:22
The Maryland portion of the watershed comprises the second-largest watershed in Montgomery County, about 60 sq mi (160 km2). About 21 percent of the creek's watershed is in Washington. Total land usage in the watershed is 896 acres (3.63 km2) of wetlands or water, 22,272 acres (90.13 km2) of residential and commercial areas, 15,488 acres (62.68 km2) of forest or grasslands, and 10,304 acres (41.70 km2) of agricultural areas. The creek has a fairly steep gradient, with rapid changes in elevation. The man-made Lake Needwood is located on the creek, north of Rockville.
In Maryland, most of the northern Rock Creek watershed has good to excellent water quality, according to studies conducted by the county government. In 2004, to preserve water quality in partially developed areas, the county imposed restrictions on development (i.e., designation of "Special Protection Areas") in parts of this sub-watershed. The southern portion of the Maryland watershed is highly urbanized. Most of this portion of the creek and its tributaries have poor water quality. The county is managing several stream restoration projects throughout the watershed.
The D.C. segment of Rock Creek also has poor water quality. In addition to typical urban stormwater pollution problems such as runoff from streets and other impervious surfaces, the creek has high bacteria levels due to combined sewer overflows (CSOs). The D.C. government, which has a stormwater discharge permit from the United States Environmental Protection Agency, is improving its stormwater management to raise water quality in Rock Creek. In 2009, the District of Columbia Water and Sewer Authority began a planned two-year effort to replace portions of the combined sewer with separate storm sewers, and so eliminate CSO-related problems in the creek.
In 2006, the National Park Service finished a project to remove or bypass eight fish barriers in the creek by adding a fish ladder to bypass the 1905 Peirce Mill Dam, modifying historic fords, and removing abandoned sewage lines and fords. The effort is designed to restore American shad, river herring, and other migratory fish to the creek and their historic upriver spawning grounds. An estimated two million fish migrate up the creek each year.
The D.C. government completed a restoration project on the Milkhouse Run and Bingham Run tributaries in 2013. As of 2014, ongoing restoration projects in the watershed include the Broad Branch and Klingle Run tributaries.
(Listed in order from the mouth upstream)