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Soil Survey of Lincoln County, West Virginia - Soil Data Mart - US ...

Soil Survey of Lincoln County, West Virginia - Soil Data Mart - US ...

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<strong>Soil</strong> <strong>Survey</strong> <strong>of</strong> <strong>Lincoln</strong> <strong>County</strong>, <strong>West</strong> <strong>Virginia</strong><br />

This map unit makes up about 34 percent <strong>of</strong> the county. It is about 40 percent<br />

Rayne and similar soils, 21 percent Gilpin and similar soils, 19 percent Matewan and<br />

similar soils, and 20 percent soils <strong>of</strong> minor extent (fig. 4).<br />

Rayne soils are deep and well drained. They are on slightly linear to convex middle<br />

and lower side slopes and on benches. Slopes range from 35 to 65 percent. These<br />

soils formed in loamy residuum and are underlain by interbedded shale, siltstone, and<br />

fine grained sandstone. Typically, they have a surface layer <strong>of</strong> silt loam and a subsoil<br />

<strong>of</strong> channery silt loam or silty clay loam. Permeability is moderate.<br />

Gilpin soils are moderately deep and well drained. They are on convex, strongly<br />

sloping summits <strong>of</strong> ridges, on linear to slightly convex side slopes <strong>of</strong> hills, and on<br />

convex shoulder slopes. Slopes range from 15 to 65 percent but are dominantly 35 to<br />

65 percent. These soils formed in loamy residuum and are underlain by interbedded<br />

shale, siltstone, and fine grained sandstone. Typically, they have a surface layer <strong>of</strong> silt<br />

loam and a subsoil <strong>of</strong> silt loam or silty clay loam. Permeability is moderate.<br />

Matewan soils are moderately deep and are well drained or somewhat excessively<br />

drained. They are on convex nose slopes, shoulders, and side slopes <strong>of</strong> hills. Slopes<br />

range from 25 to 65 percent but are dominantly 35 to 65 percent. These soils formed<br />

in channery, loamy residuum and are underlain by sandstone and siltstone. They<br />

generally are associated with areas <strong>of</strong> rock outcrop. Typically, they have a surface<br />

layer <strong>of</strong> sandy loam and a subsoil <strong>of</strong> channery or very channery sandy loam.<br />

Permeability is moderately rapid or rapid.<br />

Of minor extent in this map unit are the Upshur, Latham, and Lily soils on hills;<br />

Shelocta soils on footslopes; and Sensabaugh soils on flood plains. A few small urban<br />

areas are near major streams.<br />

The major soils in this map unit are not suited to cultivated crops, hay, or pasture<br />

but are well suited to woodland and habitat for woodland wildlife. Native trees are<br />

predominantly white oak, black oak, yellow-poplar, American beech, black walnut, red<br />

maple, and hickory. <strong>Virginia</strong> pine and shortleaf pine are in a few small areas.<br />

Figure 4.—Typical pattern <strong>of</strong> soils and parent material in an area <strong>of</strong> the Rayne-Gilpin-Matewan<br />

general soil map unit.<br />

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