11.04.2013 Views

Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

Soil Survey of Murray and Whitfield Counties, Georgia

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

168 <strong>Soil</strong> <strong>Survey</strong><br />

Depth to seasonal high water table: More than 6.0 feet<br />

Permeability: Moderately rapid<br />

Slope range: 5 to 70 percent<br />

Classification: Loamy-skeletal, mixed, semiactive, mesic, shallow Typic Dystrudepts<br />

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

Jefferson, Junaluska, <strong>and</strong> Lily soils, which have less than 35 percent rock fragments<br />

in the control section <strong>and</strong> are deeper than 20 inches to bedrock<br />

Shelocta soils, which are very deep <strong>and</strong> are on footslopes <strong>and</strong> benches<br />

Suches soils, which are very deep, are well drained, <strong>and</strong> are on flood plains<br />

Tsali soils, which have an argillic horizon <strong>and</strong> have less than 35 percent rock<br />

fragments in the control section<br />

Typical Pedon<br />

Cataska channery silt loam, 5 to 25 percent slopes; 1.0 mile east on <strong>Georgia</strong> Highway<br />

52 from intersection <strong>of</strong> U.S. Highway 411 <strong>and</strong> <strong>Georgia</strong> Highway 52, about 5.0 miles<br />

north on Holly Creek <strong>and</strong> Cool Springs Road, 3.0 miles east on dirt road, north <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 46 minutes 51 seconds N. <strong>and</strong> long. 84 degrees 42 minutes 04<br />

seconds W.<br />

A—0 to 2 inches; very dark grayish brown (10YR 3/2) channery silt loam; weak fine<br />

granular structure; very friable; many very fine, fine, medium, <strong>and</strong> coarse roots; 15<br />

percent phyllite channers; very strongly acid; clear smooth boundary.<br />

Bw—2 to 16 inches; yellowish brown (10YR 5/4) very channery silt loam; weak fine<br />

granular structure <strong>and</strong> weak fine subangular blocky structure; very friable; many<br />

very fine <strong>and</strong> fine, common medium, <strong>and</strong> few coarse roots; 35 percent phyllite<br />

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

Cr—16 to 27 inches; grayish, rippable phyllite bedded at angles up to 45 degrees;<br />

abrupt wavy boundary.<br />

R—27 inches; hard, grayish, fractured phyllite; bedded at angles up to 45 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: 20 to more than 60 inches<br />

Content <strong>of</strong> rock fragments: 15 to 45 percent in the A horizon <strong>and</strong> 35 to 45 percent in<br />

the Bw horizon<br />

Reaction: Very 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> 2 or 3<br />

Bw horizon:<br />

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

Texture—very channery silt loam or very channery loam<br />

Cr horizon:<br />

Type <strong>of</strong> bedrock—multicolored, rippable phyllite bedded at angles from 10 to 90<br />

degrees<br />

R horizon:<br />

Type <strong>of</strong> bedrock—multicolored, hard, fractured phyllite bedded at angles from 10<br />

to 90 degrees

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!