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Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

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<strong>Murray</strong> <strong>and</strong> <strong>Whitfield</strong> <strong>Counties</strong>, <strong>Georgia</strong> 191<br />

Edneytown, Jefferson, <strong>and</strong> Shelocta soils, which have bedrock at a depth <strong>of</strong> more<br />

than 60 inches<br />

Lily soils, which have lithic metas<strong>and</strong>stone bedrock at a depth <strong>of</strong> 20 to 40 inches<br />

Pigeonroost soils, which have B horizons with a hue <strong>of</strong> 7.5YR or yellower <strong>and</strong> have<br />

metamorphic or igneous bedrock at a depth <strong>of</strong> 20 to 40 inches<br />

Typical Pedon<br />

Junaluska loam, 5 to 25 percent slopes; 1.0 mile east on <strong>Georgia</strong> Highway 52 from the<br />

intersection with U.S. Highway 411 in Chatsworth, <strong>Georgia</strong>, 5.0 miles north on Holly<br />

Creek <strong>and</strong> Cool Springs Road, 2.9 miles east on dirt road, site is 200 feet south <strong>of</strong><br />

road; <strong>Murray</strong> County, <strong>Georgia</strong>; USGS topographic quadrangle, Cr<strong>and</strong>all, GA (1979);<br />

lat. 34 degrees 47 minutes 42 seconds N. <strong>and</strong> long. 84 degrees 42 minutes 02<br />

seconds W.<br />

Ap—0 to 5 inches; brown (7.5YR 4/4) loam; weak fine granular structure; very friable;<br />

many very fine, fine, medium, <strong>and</strong> coarse roots; few fine flakes <strong>of</strong> mica; 14 percent<br />

channers <strong>of</strong> phyllite; very strongly acid; gradual wavy boundary.<br />

Bt1—5 to 16 inches; strong brown (7.5YR 4/6) channery silty clay loam; weak fine <strong>and</strong><br />

medium subangular blocky structure; friable; many very fine <strong>and</strong> fine <strong>and</strong> few<br />

medium <strong>and</strong> coarse roots; few fine flakes <strong>of</strong> mica; 25 percent channers <strong>of</strong> phyllite;<br />

very strongly acid; gradual wavy boundary.<br />

Bt2—16 to 29 inches; yellowish red (5YR 5/8) channery silty clay loam; weak medium<br />

subangular blocky structure; friable; few fine flakes <strong>of</strong> mica; 20 percent channers <strong>of</strong><br />

phyllite; very strongly acid; clear wavy boundary.<br />

Cr—29 to 60 inches; multicolored fractured phyllite <strong>and</strong> metas<strong>and</strong>stone bedrock<br />

bedded at angles up to 30 degrees.<br />

Range in Characteristics<br />

Thickness <strong>of</strong> the solum: 0 to 39 inches<br />

Depth to s<strong>of</strong>t bedrock: 20 to 40 inches<br />

Depth to hard bedrock: More than 40 inches<br />

Content <strong>of</strong> rock fragments: 10 to 35 percent throughout<br />

Reaction: Very strongly acid throughout<br />

A horizon:<br />

Color—hue <strong>of</strong> 7.5YR or 10YR, value <strong>of</strong> 3 to 5, <strong>and</strong> chroma <strong>of</strong> 3 to 6<br />

Bt horizon:<br />

Color—hue <strong>of</strong> 2.5YR to 7.5YR, value <strong>of</strong> 4 or 5, <strong>and</strong> chroma <strong>of</strong> 4 to 8<br />

Texture—channery s<strong>and</strong>y clay loam, channery silty clay loam, silty clay loam, or<br />

clay loam<br />

Cr horizon:<br />

Type <strong>of</strong> bedrock—multicolored, fractured phyllite <strong>and</strong> metas<strong>and</strong>stone bedded at<br />

angles ranging from 10 to 90 degrees<br />

Ketona Series<br />

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

L<strong>and</strong>form: Flood plains, flats, <strong>and</strong> depressions<br />

Parent material: Alluvium <strong>and</strong> residuum from limestone<br />

Depth class: Very deep<br />

Drainage class: Poorly drained<br />

Seasonal high water table: Apparent; at a depth <strong>of</strong> 0.5 to 1.0 foot<br />

Permeability: Slow

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