Ellanor C. Lawrence Park is located in the Piedmont region nestled between the Blue Ridge Mountains and the coastal plain of Northern Virginia. Situated in the Culpeper Basin, the park is characterized by Triassic red bed soils in the western and central portions and thermally metamorphosed sandstone in the east. The elevation of the park is between 225 and 370 feet above sea level. The landscape is relatively flat except for the steep slopes associated with the stream valleys.
The long history of interaction between the land and its people has affected the ecosystems in the park. Ecosystems consist of upland and bottomland forest, streams, meadows and a pond.
The parkís 2nd and 3rd growth forest includes coniferous, mixed deciduous/coniferous, and deciduous stands. There are two coniferous stands in the park. One consists of dense eastern red cedar that has reclaimed an old field and the other is primarily Virginia pine. As a pioneer species, the Virginia pine colonizes areas that were once cleared for farming. Mixed pine and deciduous stands are also common. Virginia pine stands can be found among the oaks and hickories. In these areas forest succession is occurring in various stages. Eventually, young oaks and hickories will overtake the Virginia pine.
Mature Oak/Hickory stands are found in some upland areas of the park. A significant transition occurs from the upland forest to the bottomland forest along stream valleys. Here, sycamore, birch, oak, maple, and tulip trees dominate the forest canopy. Christmas ferns and spicebush grow along the stream banks.
There are also a significant number of Virginia pine blow downs in these areas as a result of storms in the early and mid 1990ís. Forest succession is slowed in these areas from the lack of hardwood regeneration. The blow downs are extremely dense and restrict animal movement.Park staff may be removing Virginia pine blow downs to promote oak and hickory growth and to reduce the excessive amount of fuel for forest fires. Invasive and exotic species are being mechanically removed where possible to increase diversity and an abundance of native plants and shrubs.
The park lies within the Chesapeake Bay watershed. It is drained by approximately five streams which range from first to third orders. Big Rocky Run, Walney Creek, and Round Lick Run are the primary drainages. Park staff monitor the biological indicators of Walney Creek and Big Rocky Run to determine their ecological health. The Walney Creek watershed is contained entirely within the park and is relatively free from human disturbances. It is a non-impaired, ecologically healthy stream that supports a variety of sensitive species at different trophic levels. Big Rocky Run flows from east to west through the southern portion of the park and is a moderately impaired stream. Although it supports a high number of fish species, the variety and number of macroinvertebrate organisms are few.
The physical characteristics and local land uses affect a streamís ecological health. Development along the Big Rocky Run watershed has impacted the physical characteristics of the habitat. During periods of heavy rain and snowmelt, storm water runoff increases the water flow causing bank erosion, channel deepening and widening, silt deposition, and temperature fluctuation. A chemical monitoring program is being initiated to monitor potential nutrient loading from non-point pollution sources for both streams. Riparian restoration projects are also being considered to help increase the overall health of Big Rocky Run.
Contrasting sharply with the adjacent oak/hickory forest, the parkís meadows provide grass dominant and forest edge habitats. In grass dominant ecosystems, grasses provide the framework on which plant and animal communities are built. The grasses in the meadow consist of fescue, bluestem, indian, eastern gamma, switch, and purple top. Various species of wildflowers bloom from early spring to late fall .
Virginia pine and black locust trees stand out in some areas amidst the grasses and wildflowers that characterize the meadow. Meadows are located in the north of the park along the gas line easement and adjacent to the Cabellís Mill/Middlegate complex. The meadow at Middlegate is managed through prescribed burns and relief cuttings which stimulate grass and wildflower growth, reduce the number of non-native plant species and eliminate the accumulation of fuel to prevent uncontrolled fires.
Walney Pond is a one acre man-made containment pond that was excavated in the 1950ís. As part of the rural landscape, for many years it was used as a local fishing hole and sometimes for ice skating. By the early 1990ís, the pond had filled in with sediment.
The pond had to be drained as part of a sewer line replacement project in 1995. The Park Authority took advantage of this opportunity to remove accumulated sediments, re-grade and reshape the features. The pond is now larger, deeper (13ft), and shaped differently.
A variety of native aquatic and emergent plants, shrubs, and trees were planted. A marsh like setting exists in the shallow end of the pond.
Largemouth bass, channel catfish, and sunfish are restocked. Special features include a picnic shelter, a boardwalk, two deck platforms, nest boxes, and informational and interpretive signs.
The pondís main source of water is surface runoff from a housing development adjacent to the park. There are concerns that excessive nutrient loads from lawn fertilizer has contributed to the heavy algal and submerged aquatic vegetation growth in the pond in the late 1990ís. Park staff has taken steps in the last several years to improve the overall health of the pond.
With periodic renovations it is hoped that Walney Pond will continue to serve the community through provision of wildlife habitat, environmental education, recreation, and as part to the landscape.