Russell County, Virginia

Survey Area VA167 Virginia

The dominant drainage class is Well drained and the dominant hydrologic group is B (moderate infiltration). The most common soil order is Ultisols — strongly weathered soils with clay-enriched subsoils, common in warm humid climates. This report summarizes the major soil map units across the survey area to help you understand what to expect when buying, building, or gardening in Russell County, Virginia. Search your address to find the exact soil composition, drainage, and series details at your specific location.

Soil Map UnitAcresDrainageHydro GroupDwellingsSeptic
Berks-Westmoreland complex, 55 to 70 percent slopes 26K Well drainedBVery limitedVery limited
Watahala gravelly silt loam, 15 to 25 percent slopes 17K Well drainedBVery limitedVery limited
Carbo-Rock outcrop complex, 25 to 65 percent slopes, eroded 17K Well drainedDVery limitedVery limited
Highsplint-Shelocta complex, 55 to 80 percent slopes, very stony 14K Well drainedAVery limitedVery limited
Watahala gravelly silt loam, 25 to 35 percent slopes 13K Well drainedBVery limitedVery limited
Berks-Chiswell complex, 55 to 80 percent slopes 12K Well drainedBVery limitedVery limited
Watahala gravelly silt loam, 35 to 55 percent slopes 10K Well drainedBVery limitedVery limited
Carbo-Rock outcrop complex, karst, 8 to 35 percent slopes, eroded 9K Well drainedDVery limitedVery limited
Berks-Westmoreland complex, 35 to 55 percent slopes 8K Well drainedBVery limitedVery limited
Carbo-Rock outcrop complex, 8 to 25 percent slopes, eroded 8K Well drainedDVery limitedVery limited
Shelocta-Highsplint complex, 35 to 55 percent slopes, very stony 7K Well drainedBVery limitedVery limited
Tumbling loam, 15 to 25 percent slopes 7K Well drainedBVery limitedVery limited
Carbo-Beech Grove complex, 15 to 25 percent slopes, very rocky, eroded 6K Well drainedDVery limitedVery limited
Berks-Poplimento complex, 15 to 35 percent slopes 6K Well drainedBVery limitedVery limited
Bland-Rock outcrop complex, 25 to 50 percent slopes, eroded 6K Well drainedCVery limitedVery limited
Frederick silt loam, 15 to 25 percent slopes, eroded 6K Well drainedBVery limitedVery limited
Lobdell-Orrville complex, 0 to 3 percent slopes, occasionally flooded 5K Moderately well drainedCVery limitedVery limited
Frederick silt loam, 8 to 15 percent slopes, eroded 4K Well drainedBSomewhat limitedSomewhat limited
Tumbling loam, 7 to 15 percent slopes 4K Well drainedBSomewhat limitedSomewhat limited
Berks-Gilpin complex, 55 to 70 percent slopes 4K Well drainedBVery limitedVery limited

Soil Orders in This Area

The USDA classifies every soil into one of 12 soil orders. Here are the dominant orders found in this survey area.

Ultisols
Strongly weathered clay soils of the Southeast. Acidic and naturally low in nutrients. Clay subsoil can slow drainage.
Inceptisols
Young but developing soils found in mountains and river terraces. Variable properties — check drainage and bedrock depth.
Alfisols
Moderately weathered forest soils with clay-enriched subsoil. Productive for agriculture, generally good for building and septic.
Entisols
Young soils with little development — found on floodplains, dunes, and steep slopes. Properties vary widely by setting.

What This Means

Building & Foundations

About 95% of soils are rated "very limited" for dwellings with basements. Specific challenges include shallow bedrock, steep slopes, flood-prone areas. A geotechnical assessment is recommended before building.

Septic Systems

About 95% of soils are rated "very limited" for septic absorption fields. Despite good drainage overall, limitations may stem from shallow bedrock, steep slopes, or seasonal conditions. Engineered or alternative systems are frequently required. Always get a professional perc test before purchasing land that needs septic.

Gardening & Agriculture

Well-drained soils on sloped terrain — good for most plants but watch for erosion. Terracing, contour planting, and mulching help retain moisture and topsoil. Drip irrigation is more effective than sprinklers on slopes.

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