Piedmont / Mountain Swamp Forests
This group contains seasonally flooded deciduous forests of backswamps and sloughs in the floodplains of northern and western Piedmont and mountain-region rivers and large streams. Communities of this group are most common in the broad, clay-rich floodplain deposits of Piedmont Mesozoic basins, but occur locally throughout the northernl and western parts of Virginia. Habitats generally have some hummock-and-hollow microtopography, with maximum flooding depths in hollows of 50 to 70 cm (20 to 28 in). Soils are usually white- or orange-mottled clay loams and loamy clays, with moderately low to moderately high base status.
Characteristic trees of these swamps include pin oak (Quercus palustris), swamp white oak (Quercus bicolor), willow oak (Quercus phellos), green ash (Fraxinus pennsylvanica), red maple (Acer rubrum), American elm (Ulmus americana) and sweetgum (Liquidambar styraciflua). In the larger river backswamps, where flooding depths may exclude oaks, stands are usually dominated by combinations of silver maple (Acer saccharinum), red maple, and green ash. Small trees and shrubs include winterberry (Ilex verticillata), common elderberry (Sambucus canadensis), silky dogwood (Cornus amomum ssp. amomum), and American hornbeam (Carpinus caroliniana ssp. caroliniana and ssp. virginiana). High-climbing woody vines, including poison ivy (Toxicodendron radicans ssp. radicans), grapes (Vitis spp.), and trumpet-creeper (Campsis radicans), are also typical. The herb layers of these communities are quite species-rich because of microtopographic diversity, but species tolerant of seasonal inundation are prevalent, including lizard's-tail (Saururus cernuus), false nettle (Boehmeria cylindrica), wood reedgrass (Cinna arundinacea), winged monkey-flower (Mimulus alatus), and various sedges (e.g ., Carex tribuloides var. tribuloides, Carex typhina, Carex squarrosa, Carex grayi). Large, well-developed swamp forests are somewhat uncommon in the Piedmont and rare in the mountains. Some of them have been destroyed or hydrologically altered by dams and reservoirs.
Reference: Fleming (2002a), Fleming and Patterson (2004).Click on the images below to open a larger image in a separate window.
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