Visitor Center Museum Closed During Construction Project
The museum at the Henry Hill Visitor Center is closed due to the installation of a fire protection system in the exhibit area. The visitor center and gift shop remain open daily and the park film is shown hourly. More »
Manassas National Battlefield Park is located in the Piedmont physiographic province (Fennemann 1938), approximately 2.5 miles northwest of Manassas City and 26 miles west of Washington, D.C. Most of the Park is in eastern Prince William County, with a very small portion extending into Fairfax County. The park is situated in the Culpeper Basin, a large Mesozoic trough that stretches across the central Piedmont from Culpeper County north through Fauquier, Prince William, and Loudoun Counties into Maryland (Lee 1979). The Culpeper Basin is a distinctive regional landscape with relatively low relief and gently rolling to nearly level topography. The park is very representative of the region, with broad, low ridges, extensive upland "flats" and shallow, sluggish drainageways.
Streams of the park are part of the Occoquan River watershed, which is part of the Chesapeake Bay watershed. Bull Run, one of the largest secondary streams of the region, borders much of the eastern edge of the Park. The watershed of Youngs Branch, a major Bull Run tributary, drains most of the park. Well-developed floodplain landforms, including depositional bars, levees, and backswamps, occur only along Bull Run. Floodplains along Young's Branch and several of its larger tributaries are much smaller and lack the microtopographic diversity of large-stream and river floodplains. Headwater drainages throughout the park are characterized by very small, sometimes braided channels with little alluvial deposition, and are flanked by flats with ephemeral or seasonal flooding controlled by fluctuating groundwater. Similar but isolated, groundwater-influenced depressions are also scattered through the park.
Fenneman, N.M. 1938. Physiography of the eastern United States. McGraw-Hill Book Company, New York. 714 pp.
Fleming, G.P. and J.T. Weber. 2003. Inventory, classification, and map of forested ecological communities at Manassas National Battlefield Park, Virginia. Natural Heritage Tech. Rep. 03-7. Virginia Department of Conservation and Recreation, Division of Natural Heritage, Richmond. Unpublished report submitted to the National Park Service. 101 pp. plus appendix.
Lee, K.Y. 1979. Triassic-Jurassic geology of the northern part of the Culpeper basin, Virginia and Maryland. U.S. Geological Survey Open-File Report 79-1557, 29 pp., 16 pl., scale: 1:24,000.
Did You Know?
Confederate troops destroyed the Stone Bridge over Bull Run in March 1862 before falling back to a more defensible position fifty miles to the south near Fredericksburg. The current structure was completed in the 1880s, on the site of the war-time bridge.