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 »
Land Use History
The natural vegetation of Manasass National Park was broadly described by Braun (1950) as belonging to the Piedmont Section of the Oak-Chestnut Forest Region. Centered in the Appalachian Mountains, this vegetation unit was formerly characterized by various mixtures of oaks and American chestnut, with small inclusions of pines on xeric ridges and mixed mesophytic forest in coves, ravines, and stream bottoms. Following the removal of American chestnut as an overstory tree by an introduced fungal blight during the early decades of the 20th century, this region is now broadly characterized as mixed oak forest (Stephenson et al. 1993) or oak-hickory-pine forest (Küchler 1964). It is worth noting that because of its low relief and distinctive soils, the original vegetation of the Culpeper Basin was probably dissimilar to most other parts of the Oak-Chestnut Forest Region. Today, there is little evidence that chestnut was important in the Basin, and the general vegetation of the area may have been closer to Braun's more western Oak-Hickory Forest Region. In addition, the relatively flat, poorly drained soils of the Basin have no doubt always supported unique communities with an abundance of pin oak, swamp white oak, and other species that are decidedly less common in other physiographic subregions of the Piedmont province. Here, the moist flats on the "Piedmont Lowland" of Virginia are "quite different, with pin oak, red maple, willow oak, swamp white oak, and sweet gum" (Braun, 1950).
Many of the rare species of the park, e.g., blue-hearts, hairy beardtongue, marsh hedgenettle, and buffalo clover, have affiliations with prairie vegetation west of the Appalachians (Belden et al. 1998). The presence of these disjunct or peripheral species might be explained by accounts of early explorers and settlers, which indicate that the Culpeper Basin originally had extensive natural savannas and grasslands (Allard and Leonard 1962, Brown 2000). These prairie-like habitats probably remained open over the long term because of frequent fires, both natural and controlled by Native Americans, that traveled unobstructed across the gentle terrain of the Basin (Maxwell 1910, Van Lear and Waldrop 1989). Plastic hardpan soils, weathered from diabase and locally known as "Jackland" because of the abundance of blackjack oaks on them, were probably the most favorable for development of these grassland openings.
The park's land and most other parts of the Culpeper Basin have been settled for almost three centuries. In the post-settlement era, the original grasslands were destroyed by extensive clearing and agriculture, widespread fire suppression, and repeated cutting, which has resulted in dense secondary forests. The mosaic of agricultural fields and secondary forests in the study area has shifted considerably even since the Civil War. A number of sites that were cleared at the time of the Civil War battles are now reforested, and other historically forested sites have since been cleared. Some areas of Stuarts Hill, Bald Hill, the ridges east of Brawner Farm and south of Battery Heights, and the ridge north of Groveton have been continuously forested (although cut) since the time of the Civil War. Old fields undergoing secondary succession in this area are generally characterized by stands of Virginia Pine, eastern red cedar, flowering dogwood, and fast-growing hardwoods such as white ash and tulip-poplar.
In recent years, large portions of the Culpeper Basin in Fairfax, Loudoun, Prince William, and Fauquier Counties have been subjected to intense development pressure as the Washington, D.C. area's growth has expanded westward. As a result, many of the region's finest natural areas have been destroyed or threatened. Increasingly, Manassas National Battlefield Park is becoming a natural area oasis as development spreads from nearby Manassas. Because of a mandate to maintain the Park's landscape in its Civil War-era condition, ambitious restoration plans are underway.
Allard, H.A. and E.C. Leonard. 1962. List of vascular plants of the Northern Triassic area of Virginia. Castanea 27: 1-56.
Belden, A. Jr., G.P. Fleming, and N.E. Van Alstine. 1998. A natural heritage inventory of Manassas National Battlefield Park. Nat. Heritage Tech. Rep. 98-7. Virginia Dept. of Conservation and Recreation, Division of Natural Heritage, Richmond, VA. 67 pp. plus appendices.
Braun, E.L. 1950. Deciduous forests of eastern North America. Macmillan Publishing Co., New York. 596 pp.
Brown, H. 2000. Wildland burning by American Indians in Virginia. Fire Management Today 60:3.
USDA Forest Service, Washington, D.C.
Küchler, A.W. 1964. Potential natural vegetation of the conterminous United States. American Geographical Society Special Publication 36.
Maxwell, H. 1910. The use and abuse of forests by the Virginia Indians. William and Mary College Quarterly Historical Magazine XIX: 73-103.
Stephenson, S.L., A.N. Ash, and D.F. Stauffer. 1993. Appalachian oak forests. Pages 255-303 in W.H. Martin, S.G. Boyce, and A.C. Echternacht (eds.). Biodiversity of the Southeastern United States: upland terrestrial communities. John Wiley & Sons, Inc., New York.
Van Lear, D.H. and T.A. Waldrop. 1989. History, uses, and effects of fire in the Appalachians. USDA Forest Service General Tech. Rep. SE-54. Southeastern Forest Experiment Station, Clemson, S.C. 20 pp.
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.