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<br />JERRY SERIES <br />The Jerry series is a member.of the fine, <br />montmorillonitic family of Argic Cryoborolls. Typically, <br />Jerry soils have dark grayish brown soils in their A, B, <br />and C horizons. They have friable, medium fine granular, <br />loamy A horizons; friable, medium fine, sub angular blocky, <br />clayey B horizons; and friable, aubangular blocky to massive, <br />clay to heavy clayey loam C horizons. <br />The Jerry series are deep, well-drained soils that formed <br />in residuum and colluvium from sandstone bedrock. They occur <br />on steep mountain slopes. These soils have slow permeability <br />• and slow runoff. <br />Typifying Pedon: Jerry loam, fine mixed (colors are for <br />dry soils unless otherwise noted). <br />A (0-4"): Dark grayish brown (10YR 5/2) loam, very <br />dark gray brown (10YR 3/2) moist; moderately fine granular <br />structure; loose, triable, sticky and plastic; 10~ stone, <br />25~ gravel; noneffervescent; mildly alkaline (pH 7.5); clear <br /> <br />wsvy boundary. <br />B (4-9"): Dark grayish brown (10YR 5/2) clayey loam, <br />very dark gray brown (10YR 3/2) moist; moderately fine <br />subangular and blocky structure; hard, friable, sticky and <br />plastic;.10~ gravel; nonefferevescent; mildly alkaline (pH <br />7.5); clear wavy boundary. <br /> <br />