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Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

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88 <strong>Soil</strong> <strong>Survey</strong><br />

Urban l<strong>and</strong><br />

Urban l<strong>and</strong> consists <strong>of</strong> areas that have been altered by cutting, filling, <strong>and</strong> shaping.<br />

Schools, parking lots, streets, commercial buildings, residential dwellings, or other<br />

structures are located in these areas.<br />

<strong>Soil</strong> Properties <strong>and</strong> Qualities<br />

Drainage class: Minvale—well drained<br />

Seasonal high water table: Minvale—more than 6.0 feet<br />

Permeability: Minvale—moderate<br />

Available water capacity: Minvale—moderate<br />

Root zone: Minvale—very deep<br />

Minor Components<br />

Bodine, Fullerton, Holston, Shack, <strong>and</strong> Waynesboro soils, which are in similar<br />

l<strong>and</strong>form positions<br />

Wax soils, which are in the slightly lower l<strong>and</strong>form positions<br />

<strong>Soil</strong>s that formed in alluvial sediments along drainageways<br />

Use <strong>and</strong> Management<br />

L<strong>and</strong> use: Minvale—lawns, gardens, <strong>and</strong> idle acres; Urban l<strong>and</strong>—buildings, streets,<br />

parking lots, sidewalks, <strong>and</strong> other structures<br />

Urban development<br />

Suitability: Moderately suited<br />

Limitations: Slow water movement <strong>and</strong> slope<br />

Recreational development<br />

Suitability: Moderately suited<br />

Limitations: Slope <strong>and</strong> content <strong>of</strong> gravel<br />

Interpretive Group<br />

L<strong>and</strong> capability classification: Minvale—4E; Urban l<strong>and</strong>—none assigned<br />

MoF—Montevallo very channery loam, 30 to 60 percent<br />

slopes<br />

Setting<br />

L<strong>and</strong>form: Hills <strong>and</strong> ridges<br />

L<strong>and</strong>form position: Summits, shoulders, <strong>and</strong> backslopes<br />

Surface features: Shale <strong>and</strong> dissected quartzite fragments on the surface<br />

Flooding: None<br />

Slope: Steep<br />

Typical Pr<strong>of</strong>ile<br />

Surface layer:<br />

0 to 5 inches—dark yellowish brown very channery loam<br />

Subsoil:<br />

5 to 10 inches—yellowish brown very channery loam<br />

Underlying material:<br />

10 to 60 inches—multicolored, rippable shale bedrock bedded at angles up to 70<br />

degrees

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