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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> 215<br />

roots; 30 percent phyllite <strong>and</strong> metas<strong>and</strong>stone channers; very strongly acid; clear<br />

wavy boundary.<br />

Bt—4 to 14 inches; yellowish red (5YR 5/6) clay loam; weak medium subangular<br />

blocky structure; friable; common very fine <strong>and</strong> fine <strong>and</strong> few medium <strong>and</strong> coarse<br />

roots; many faint <strong>and</strong> common distinct clay films on faces <strong>of</strong> peds; 10 percent<br />

phyllite <strong>and</strong> metas<strong>and</strong>stone channers; strongly acid; clear wavy boundary.<br />

Cr—14 to 60 inches; multicolored, rippable, interbedded phyllite <strong>and</strong> metas<strong>and</strong>stone<br />

bedded at angles up to 60 degrees<br />

Range in Characteristics<br />

Thickness <strong>of</strong> the solum: 10 to 20 inches<br />

Depth to s<strong>of</strong>t bedrock: 10 to 20 inches<br />

Depth to hard bedrock: More than 30 inches<br />

Content <strong>of</strong> rock fragments: 0 to 35 percent in all horizons<br />

Reaction: Very strongly acid or strongly acid throughout<br />

A horizon:<br />

Color—hue <strong>of</strong> 7.5YR or 10YR, value <strong>of</strong> 3 or 4, <strong>and</strong> chroma <strong>of</strong> 3 to 6<br />

Bt horizon:<br />

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

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

loam<br />

Cr horizon:<br />

Type <strong>of</strong> bedrock—multicolored, rippable, interbedded metasedimentary <strong>and</strong><br />

phyllite rocks bedded from 10 to 90 degrees<br />

Wax Series<br />

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

L<strong>and</strong>form: Drainageways<br />

Parent material: Loamy alluvium from cherty limestone<br />

Depth class: Moderately deep<br />

Drainage class: Moderately well drained<br />

Seasonal high water table: Perched; at a depth <strong>of</strong> 1.5 to 3.0 feet<br />

Permeability: Slow<br />

Slope range: 0 to 6 percent<br />

Classification: Fine-loamy, siliceous, thermic Typic Fragiudults<br />

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

Bodine soils, which are somewhat excessively drained, have more than 35 percent<br />

chert fragments throughout the pr<strong>of</strong>ile, do not have fragic properties, <strong>and</strong> are on<br />

adjacent upl<strong>and</strong>s<br />

Dewy soils, which have more than 35 percent clay in the control section, are well<br />

drained, do not have fragic properties, <strong>and</strong> are on adjacent upl<strong>and</strong>s<br />

Guthrie soils, which are poorly drained<br />

Fullerton soils, which have more than 35 percent clay in the control section, are well<br />

drained, do not have fragic properties, <strong>and</strong> are on adjacent upl<strong>and</strong>s<br />

Minvale soils, which have 15 to 35 percent chert fragments in the control section, are<br />

well drained, do not have fragic properties, <strong>and</strong> are in the higher l<strong>and</strong>scape positions<br />

Shack soils, which have 15 to 35 percent chert fragments in the control section <strong>and</strong><br />

are on adjacent upl<strong>and</strong>s<br />

Subligna soils, which are well drained, do not have fragic properties, <strong>and</strong> have more<br />

than 35 percent rock fragments throughout the pr<strong>of</strong>ile

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