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.

<strong>Murray</strong> <strong>and</strong> <strong>Whitfield</strong> <strong>Counties</strong>, <strong>Georgia</strong> 161<br />

<strong>and</strong> medium roots; few distinct <strong>and</strong> common faint clay films on faces <strong>of</strong> peds;<br />

common medium prominent red (2.5YR 4/8) masses <strong>of</strong> oxidized iron; very strongly<br />

acid; gradual wavy boundary.<br />

Bt2—24 to 35 inches; brownish yellow (10YR 6/8) silty clay; moderate medium<br />

subangular blocky structure; firm; few fine roots; common distinct clay films on<br />

faces <strong>of</strong> peds; few fine shale fragments; common medium prominent red (2.5YR<br />

4/8) <strong>and</strong> few fine faint strong brown (7.5YR 5/8) masses <strong>of</strong> oxidized iron; very<br />

strongly acid; gradual wavy boundary.<br />

Bt3—35 to 47 inches; brownish yellow (10YR 6/8) silty clay; moderate medium<br />

subangular blocky structure; firm; common distinct clay films on faces <strong>of</strong> peds; few<br />

fine <strong>and</strong> medium shale fragments; common medium prominent red (2.5YR 4/8)<br />

<strong>and</strong> few medium faint strong brown (7YR 5/8) masses <strong>of</strong> oxidized iron; few<br />

medium prominent very pale brown (10YR 8/2) iron depletions; very strongly acid;<br />

gradual wavy boundary.<br />

Cr—47 to 60 inches; multicolored, rippable shale bedrock.<br />

Range in Characteristics<br />

Thickness <strong>of</strong> solum: 40 to 60 inches<br />

Depth to s<strong>of</strong>t bedrock: 40 to 60 inches<br />

Depth to hard bedrock: More than 60 inches<br />

Content <strong>of</strong> rock fragments: 0 to 15 percent throughout, except the layer directly above<br />

the rippable bedrock, which ranges up to 40 percent<br />

Reaction: Very strongly acid throughout, except where lime has been applied<br />

A horizon:<br />

Color—hue <strong>of</strong> 10YR or 2.5Y, value <strong>of</strong> 4 or 5, <strong>and</strong> chroma <strong>of</strong> 2 to 4<br />

BE horizon (where present):<br />

Color—hue <strong>of</strong> 7.5YR or 10YR, value <strong>of</strong> 5 to 7, <strong>and</strong> chroma <strong>of</strong> 4 or 6<br />

Texture—silt loam or silty clay loam<br />

Mottles—common in shades <strong>of</strong> yellow<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> 6 or 8<br />

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

Mottles—few to common in shades <strong>of</strong> red, yellow, brown, <strong>and</strong> gray<br />

Bt horizon (lower 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> 6 or 8<br />

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

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

gray<br />

Cr horizon:<br />

Type <strong>of</strong> bedrock—multicolored, rippable shale<br />

Note: The Albertville soils in this survey area are taxadjuncts to the series because<br />

they have a zone <strong>of</strong> seasonal saturation (seasonal high water table) within 40 inches<br />

<strong>of</strong> the surface, which is not typical for the series. Albertville soils in the survey area are<br />

moderately well drained, whereas they are generally well drained.<br />

Allen Series<br />

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

L<strong>and</strong>form: Ridges

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

Saved successfully!

Ooh no, something went wrong!