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Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

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166 <strong>Soil</strong> <strong>Survey</strong><br />

A or Ap horizon:<br />

Color—hue <strong>of</strong> 10YR or 2.5Y, value <strong>of</strong> 3 to 6, <strong>and</strong> chroma <strong>of</strong> 2 or 3<br />

E horizon:<br />

Color—hue <strong>of</strong> 10YR or 2.5Y, value <strong>of</strong> 5 or 6, <strong>and</strong> chroma <strong>of</strong> 4<br />

Texture—extremely gravelly silt loam or very gravelly silt loam<br />

Bt horizon (upper part):<br />

Color—hue <strong>of</strong> 7.5YR or 10YR, value <strong>of</strong> 5 or 6, <strong>and</strong> chroma <strong>of</strong> 4 to 8<br />

Texture—extremely gravelly loam, extremely gravelly silty clay loam, or extremely<br />

gravelly clay loam<br />

Mottles—none to common in shades <strong>of</strong> red, yellow, <strong>and</strong> brown<br />

Bt horizon (lower part):<br />

Color—hue <strong>of</strong> 5YR to 10YR, value <strong>of</strong> 5 or 6, <strong>and</strong> chroma <strong>of</strong> 4 to 8<br />

Texture—extremely gravelly loam, extremely gravelly silty clay loam, or extremely<br />

gravelly clay loam<br />

Mottles—none to common in shades <strong>of</strong> red, yellow, <strong>and</strong> brown<br />

Capshaw Series<br />

Major l<strong>and</strong> resource area: Southern Appalachian Ridges <strong>and</strong> Valleys<br />

L<strong>and</strong>form: Stream terraces, depressions, <strong>and</strong> flats<br />

Parent material: Alluvium over clayey residuum weathered from limestone<br />

Depth class: Deep or very deep<br />

Drainage class: Moderately well drained<br />

Seasonal high water table: Apparent; at a depth <strong>of</strong> 2.0 to 3.5 feet<br />

Permeability: Slow<br />

Slope range: 0 to 6 percent<br />

Classification: Fine, mixed, semiactive, thermic Oxyaquic Hapludalfs<br />

Geographically Associated <strong>Soil</strong>s<br />

Albertville soils, which are well drained <strong>and</strong> have shale bedrock at a depth <strong>of</strong> 40 to<br />

60 inches<br />

Conasauga soils, which have shale bedrock at a depth <strong>of</strong> 20 to 40 inches<br />

Docena soils, which have a fine-silty texture<br />

Ketona soils, which are poorly drained<br />

Whitwell soils, which have less than 35 percent clay in the control section<br />

Typical Pedon<br />

Capshaw silt loam, 2 to 6 percent slopes; 0.5 mile south <strong>of</strong> <strong>Georgia</strong>-Tennessee state<br />

line on Sugar Creek Road, 1,350 feet west <strong>of</strong> road; <strong>Murray</strong> County, <strong>Georgia</strong>; USGS<br />

topographic quadrangle, Beaverdale, GA-TN (1972); lat. 34 degrees 58 minutes 48<br />

seconds N. <strong>and</strong> long. 84 degrees 48 minutes 28 seconds W.<br />

A—0 to 7 inches; brown (10YR 5/3) silt loam; many medium faint very pale brown<br />

(10YR 7/3) mottles; weak medium granular structure; very friable; many fine <strong>and</strong><br />

medium <strong>and</strong> common coarse roots; few small pebbles; strongly acid; clear smooth<br />

boundary.<br />

Bt1—7 to 14 inches; brownish yellow (10YR 6/6) silty clay loam; weak medium<br />

subangular blocky structure; friable; common fine <strong>and</strong> few medium roots; few faint<br />

clay films on faces <strong>of</strong> peds; few small pebbles; few fine distinct very pale brown<br />

(10YR 7/3) iron depletions; strongly acid; gradual wavy boundary.<br />

Bt2—14 to 22 inches; brownish yellow (10YR 6/8) silty clay; moderate medium<br />

subangular blocky structure; firm; few fine <strong>and</strong> medium roots; common faint <strong>and</strong>

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