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Soil Survey of Karnes County, Texas - Soil Data Mart - US ...

Soil Survey of Karnes County, Texas - Soil Data Mart - US ...

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<strong>Karnes</strong> <strong>County</strong>, <strong>Texas</strong> 59<br />

Figure 10.—Active erosion makes plant cover difficult to establish in this excavated area.<br />

The low available water capacity and droughtiness are<br />

limitations. Proper stocking rates, brush management,<br />

and controlled grazing can help conserve moisture<br />

and improve or maintain productivity.<br />

This soil has fair potential as openland and<br />

rangeland wildlife habitat. The low available water<br />

capacity, excess lime, and droughtiness limit the plant<br />

growth necessary for good habitat.<br />

Yields are low if this soil is used as improved<br />

pasture or cropland. The low available water capacity,<br />

low natural fertility, droughtiness, and excess lime are<br />

limitations. The hazard <strong>of</strong> water erosion is moderate.<br />

This soil is poorly suited to urban uses. Seepage,<br />

permeability, and stoniness are moderate to severe<br />

limitations for sanitary facilities. The potential for<br />

corrosion <strong>of</strong> uncoated steel is a moderate limitation for<br />

building site development.<br />

This soil is moderately suited to recreational uses.<br />

Slope and small stones are moderate limitations.<br />

This Pettus soil is in capability subclass IVe and in<br />

the Shallow Ridge range site.<br />

Px—Pits and Dumps<br />

This map unit consists <strong>of</strong> areas that have been<br />

excavated for uranium mining. They consist <strong>of</strong> mine<br />

pits that impound water and soil materials piled above<br />

ground level (fig. 10). These soil areas are prominent<br />

on the landscape.<br />

The pits range from 5 to 35 acres in size and have<br />

nearly vertical side walls. They are 100 to 250 feet<br />

deep, 200 to 800 feet wide, and 600 to 3,200 feet long.<br />

They impound water that is 50 feet deep or more.<br />

Water erosion is very active on surface soil materials<br />

and on the side walls. The walls at ground level have<br />

deep gullies. The side walls are very unstable and are<br />

in a constant process <strong>of</strong> caving in.<br />

The areas <strong>of</strong> piled soil material are 50 to 100 feet<br />

higher than the natural surface elevation. They consist<br />

<strong>of</strong> original topsoil that has been mixed with the parent<br />

material. They range from 10 to 450 acres in size.<br />

They have very steep side slopes and nearly level to<br />

gently sloping tops. The hazard <strong>of</strong> water erosion is

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