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~. <br />t <br />i .. .. _. . . 6... <br />CRYOBOROLLS <br />The Cryoborolls consist of shallow to deep, somewhat excessively <br />to well drained soils formed in residuum and from colluvium derived <br />from sandstone and shale. They generally occur on southern and <br />southeastern-facing sideslopes and have slopes of 10 to 49 percent. <br />The Cryoborolls are similar to and occur near Splitro and Roxal <br />Variant-Starman complex soils. Splitro soils have lithic contacts. <br />Roxal Variant and Starma^ soils lack mollic epipedons. They also occur <br />near Winevada, Lymanson, Owen Creek shallow Variant and <br />Torriorthents-Rock outcrop complex soils. <br />Soils of this map unit are classified at the suborder level as <br />~~ <br />LJ <br />Cryoborolls. <br />Typical pedon of Cryoborolls, 34 percent slope is located <br />within 402,000N, 1,430,000E and 405,000N, 1,434,OOOE. <br />Al--0 to 3 inches; brown (lOYR 5)3) sandy loam, dark brown (lOYR <br />3/3) moist; massive; slightly hard, friable, nonsticky and nonplastic; <br />slightly effervescent; moderately alkaline; gradual smooth boundary. <br />C1--3 to 18 inches; light yellowish brown (lOYR 6/4) very fine <br />sandy clay loam, yellowish brown <lOYR 5/4) moist; massive; slightly <br />hard, friable, nonsticky and nonplastic; strongly effervescent; <br />moderately alkaline; clear smooth boundary. <br />C1r--18 inches; weathered sandstone. <br />u <br />7-201 <br />