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t <br />COBERLY VARIANT <br />The Coberly Variant consists of deep well drained soils formed <br />from alluvial and colluvial materials derived from sandstone and shale <br />with a component of aeolian material. They are located in upland basins <br />and on rolling uplands and have slopes of 0 to 49 percent. <br />Coberly Variant soils are similar to and occur near the <br />coarse-loamy, mixed, frigid Aridic Haploborolls of map unit 41. The <br />Aridic Haploborolls have mollic epipedons that are less than 16 inches <br />deep and coarse-loamy control section textures. They also occur near <br />Savage and Rentsac Variant soils. <br />Coberly Variant soils are classified as fine-loamy, mixed Pachic <br />Haploborolls. <br />This soil is a variant because it is deeper than the acceptable <br />range in depth for the Coberly Series and has a fine-loamy control <br />section texture. <br />Typical pedon of Coberly Variant sandy clay loam, 11 percent slope <br />is located within 408,000N, 1,418,000E and 411,000N, 1,422,000E. <br />All--O to 1 inch; brown (lOYR 5/3) sandy clay loam, very dark <br />grayish brown (lOYR 3/2) moist, weak fine granular structure; loose, <br />loose, nonsticky, nonelastic; neutral; clear smooth boundary. <br />A12--1 to 6 inches; brown (lOYR 5/3) sandy clay loam, dark brown <br />(lOYR 3/3) moist; weak medium subangular blocky structure; hard, firm, <br /> <br />2-197 <br />