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 is underlain by sedimentary, metasedimentary, and igneous rocks of Triassic and Jurassic age. Siltstone of the Ball's Bluff Formation is the most extensive bedrock type in the area. This material is a red to purplish-brown, iron-rich, micaceous siltstone with thin to medium bedding that tends to produce platy to slab-like fragments when weathered. Calcium is abundant in concretions, veins, and cement. Minor interbeds of red silty shale and arkosic sandstone are also present. This formation constitutes the parent material of almost all soils in the eastern half of the park (Leavy et al 1983, Lee 1977).
The western half of the Park contains substantial areas underlain by intrusive diabase, which occurs in irregular dikes, stocks, and sills. This diabase is a dense, medium-grained, dark-gray to black mafic, igneous rock composed primarily of feldspar and pyroxene (Lee 1979). This bedrock is well expressed in a narrow dike that originates near Wellington to the south of MNBP and extends northward through the Park, passing west of Groveton and ending just SE of Sudley. Other diabase intrusions are located in the vicinity of Stuarts Hill, south of Battery Heights, and on the ridge east of Brawner Farm (Leavy et al. 1983). The soil survey for Prince William County (Elder 1989) indicates that soils derived from diabase are also located in the vicinity of Bald Hill. Thick, residual soils cover most diabase intrusions but often contain spheroidally weathered boulders at the surface.
Thermally metamorphosed sedimentary rocks surround the diabase intrusive bodies (Lee 1979). Bands of these rocks are generally less than 0.5 km wide within the Park and often much narrower. They are composed of red-brown siltstone and shale hornfels that have been altered under intense heat and pressure. Metamorphic minerals such as epidote, cordierite, pyroxene, and garnet are common along joints or fractures (Leavy et al. 1983).
Click here to learn about the National Park Service's Inventory & Monitoring Program's Paleontological Inventory of the National Capital Region: http://science.nature.nps.gov/im/units/ncrn/inventories_paleo.cfm
Elder, J.H. 1989. Soil survey of Prince William County, Virginia. U.S.D.A. Soil Conservation Service in cooperation with Virginia Polytechnic Institute and State University. U.S. Government Printing Office, Washington, D.C. 245 pp. plus maps.
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.
Leavy, B.D., A.J. Froelich, and E.C. Abram. 1983. Bedrock map and geotechnical properties of rocks of the Culpeper basin and vicinity, Virginia and Maryland. scale: 1:125,000. Map 1-1313-C. U.S. Geological Survey, Reston, VA.
Lee, K.Y. 1977. Triassic stratigraphy in the northern part of the Culpeper basin, Virginia and Maryland. U.S. Geological Survey Bulletin 1422-C, 17 p.
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?
During the First Manassas campaign, Confederate reinforcements travelled by rail from Piedmont Station to Manassas Junction. The 35 mile trip marked the first time in American history that railroads were tactically used to forward soldiers towards the frontlines of combat.