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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 />

55 counties comprising <strong>West</strong> <strong>Virginia</strong>. The county was named for Abraham <strong>Lincoln</strong>,<br />

the 16th president <strong>of</strong> the United States.<br />

The first settlements in <strong>Lincoln</strong> <strong>County</strong> were established in about 1800. There<br />

probably were fewer than a dozen families residing within the present boundaries <strong>of</strong><br />

<strong>Lincoln</strong> <strong>County</strong> in that year (Lambert 1991); however, there was a steady stream <strong>of</strong><br />

immigrants arriving in the Ohio River valley at that time. The adjacent states <strong>of</strong><br />

Kentucky and Ohio were established in 1791 and 1803, respectively. Many <strong>of</strong> the<br />

earliest settlers in <strong>Lincoln</strong> <strong>County</strong> were from the eastern or central part <strong>of</strong> <strong>Virginia</strong>.<br />

The primary settlements in the county at that time were along the Guyandotte and<br />

Mud Rivers, as well as Twelvepole Creek. The first building in the present area <strong>of</strong><br />

Hamlin was built in 1802. It was the cabin <strong>of</strong> David Stephenson.<br />

Farming<br />

In 1997, <strong>Lincoln</strong> <strong>County</strong> had 214 farms, or about 20 percent fewer farms than in<br />

1987. The average size <strong>of</strong> these farms was 128 acres (U.S. Department <strong>of</strong> Agriculture<br />

1999). A total <strong>of</strong> 8,501 acres in the county was used as cropland. Of this acreage,<br />

about 2,229 acres, or 26 percent, was used for harvested crops. The main farm<br />

products in these areas were hay, tobacco, or grain crops. Livestock or poultry was<br />

raised on nearly half <strong>of</strong> the farms. The raising <strong>of</strong> beef cattle was the leading livestock<br />

enterprise. Sheep were also commonly raised. Most <strong>of</strong> the farm income in the county<br />

was derived from the sale <strong>of</strong> beef cattle or tobacco. Most farms were operated on a<br />

part-time basis.<br />

Transportation Facilities<br />

The transportation needs <strong>of</strong> <strong>Lincoln</strong> <strong>County</strong> are served by numerous county and<br />

state roads, including routes 3, 7, 10, 15, and 214, and U.S. Route 119, which is a<br />

four-lane highway. Railroad trackage is maintained in <strong>Lincoln</strong> <strong>County</strong> along the<br />

Guyandotte and Little Coal Rivers. The railroad system is used primarily for hauling<br />

coal from the mining region in the southern part <strong>of</strong> <strong>West</strong> <strong>Virginia</strong>. <strong>Lincoln</strong> <strong>County</strong><br />

currently has no commercial airport facilities.<br />

Relief and Drainage<br />

<strong>Lincoln</strong> <strong>County</strong> is within two major land resource areas (MLRAs)—the Central<br />

Allegheny Plateau and the Cumberland Plateau and Mountains. The Central<br />

Allegheny Plateau MLRA encompasses roughly the northern half <strong>of</strong> <strong>Lincoln</strong> <strong>County</strong>.<br />

It consists <strong>of</strong> predominantly sandstone, shale, and siltstone with some layers <strong>of</strong><br />

calcareous rocks. The landscape is characterized by nearly level or gently sloping<br />

valleys and sloping to steep ridgetops that are separated by long, steep side<br />

slopes. Local relief in this part <strong>of</strong> the county generally ranges from about 400 to<br />

500 feet.<br />

The Cumberland Plateau and Mountains MLRA encompasses the southern half<br />

<strong>of</strong> the county. Geologic strata generally consist <strong>of</strong> interbedded sandstone, siltstone,<br />

and shale with some coal and limestone strata. Since the southern half <strong>of</strong> the county<br />

has a higher percentage <strong>of</strong> more resistant sandstone bedrock, it exhibits more<br />

rugged topography than the northern portion. This area is characterized by some<br />

sloping plateau remnants along the summits <strong>of</strong> ridges, but most <strong>of</strong> the area is rugged<br />

with narrow flood plains along streams and narrow, moderately steep to very steep<br />

ridgetops separated by long, very steep side slopes with numerous bedrock<br />

escarpments and rock outcroppings and stony or bouldery surfaces. Local relief in<br />

the southern part <strong>of</strong> the county generally ranges from about 600 to 800 feet.<br />

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