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<br />~ <br /> <br />LAMAR AND DELTA COUNTIES, TEXAS <br /> <br />This map unit consists of prairie soils that have a <br />, loamy sur(ace layer and a clayey subsoil. Slopes are 0 to <br />5 percent (fig. 3). This. unit makes up about 22 percent of <br />the survey areas. It is about 30 percent Wilson soils, 26 <br />percent Normangee soils, 22 percent Crockett soils, and <br />22 percent other soils. <br />, Wilson solis are nearly level to gently sloping and are <br />on ridgetops and foot slopes. These solis are somewhat <br />poorly drained. The surface layer Is very dark gray, <br />slightly acid silt loam about 6 inches thick. Between <br />depths of 6 and 9 inches, the soil Is very dark gray, <br />medium acid clay loam. Between depths of 9 and 28 <br />, inches, the soil is very dark gray, slightly acid clay. Be- <br />tween depths of 28 and 39 inches, the soil is dark gray, <br />neutral, clay. Between depths of 39 and 80 inches, the <br />soil is grayiSh brown, mildly alkaline Clay that has light <br />olive brown and olive yellow mottles. <br />Normangee soils are gently sloping and are on tops <br />and sides of ridges. These solis are moderately well <br />drained. The surface layer is dark brown, slightly acid <br />Clay loam about 7 inches thick. Between depths of 7 and <br />16 Inches, the soil is brown, medium acid clay that has <br />red, reddish brown, and dark grayish brown mottles. Be- <br />tween depths of 16 and 28 inches, the soil Is yellowish <br />brown, neutral clay that has mottles in shades of red and <br />brown. Between depths of 28 and 38 inches, the soil is <br />mottled grayish brown and light olive brown, mildly alka- <br />line clay. Between depths of 38 and 48 inches, the soil is <br />light olive brown, moderately alkaline Clay that has gray- <br />ish brown mottles. Between depths of 48 and 57 inches, <br />the soil is mottled olive, light olive brown, and yellowish <br />, brown, moderately alkaline clay. The underlying material <br />Is light olive gray, moderately alkaline weathered shale to <br />a depth of 65 Inches. II has light olive brown mottles. <br />Crockett solis are gently Sloping and are on tops and <br />sides of ridges. These soils are moderately well drained. <br />The surface is very dark grayish brown, slightly acid loam <br />about 8 inches thick. Between depths of 8 and 17 <br />Inches, the soil is mottled brown and reddish brown, <br />slightly acid clay. Between depths of 17 and 29 inches, <br />the soil is mottled light olive brown and olive, slightly <br />acid Clay. Between depths of 29 and 39 inches, the soil <br />is :olive, neutral clay that has strong brown and yellowish <br />red mottles. Between depths of 39 and 51 inches, the <br />soli is olive brown, mildly alkaline clay. Between depths <br />, of 51 and 59 inches, the soil Is light olive brown, moder- <br />, ately alkaline clay loam that has grayiSh brown and light <br />olive brown mottles. Between depths of 59 and 73 <br />inches, the soil is motiled light gray and brownish yellow, <br />moderately alkaline loam. <br />Other soils are Parisian, Mabank, Lassiter, and Roxlon <br />solis. Parisian and Mabank soils have a loamy surface <br />layer and a clayey subsoil. They are gently sloping and <br />nearly leveJ and are on uplands. The loamy Lassiter and <br /><\Iayey ROxlOn soils are frequently flooded and are on <br />bottol'!llands. ' , <br /> <br />~, <br /> <br />5 <br /> <br />The soils in this unit have high p'otential for pasjure <br />and hay. They have medium potential for crops and <br />range. They have very slow permeability, erode easily, <br />and are droughty. Potential for woodland Is low because <br />of very slow permeability. There Is no woodland grazing <br />in this unit. Soils in this unit are used mainly for range or . , <br />for pasture and hay. <br />The soils in this unit have medium potential for most <br />urban uses. Umiting factors are low strength and the <br />Shrinking and swelling with changes in moisture content. <br />The potential for recreation Is medium because of the <br />very slow permeability. <br /> <br />4. Trinity-Kaufman <br /> <br />Nearly level, vel)' slowly permeable, clayey salls on flood <br />plains <br /> <br />This map unit consists of clayey soils that crack when' <br />dry. Slopes are 0 to 1 percent. This unit makes up about <br />10 percent of the survey area It is about 59 percent <br />Trinity soils, 33 percent Kaufman soils, and 8 percent <br />other soils. <br />Trinity soils are somewhat poorly drained. The surface <br />layer is very dark gray, moderately alkaline clay about 29 <br />inches thick. Between depths of 29 and 72 inches, the <br />soil is black, moderately alkaline clay. <br />Kaufman soils are somewhat poorly drained. The sur- <br />face layer Is black, Slightly acid clay about 35 Inches <br />thick. Between depths of 35 and 80 inches, the soil ,is <br />. very dark gray, slightly acid clay that has olive brown and' <br />dark yellowish brown mottles. <br />Other soils are Varro and Elbon soils. These soils are <br />frequently flooded, loamy solis on bottom lands. <br />Soils in this unit have high potential for pasture and <br />hay, woodland, and woodland grazing. Potential for <br />crops is medium because of flooding. There is no range <br />in this unit. " . <br />The potential for urban uses and recreation is low <br />because of flooding, the clayey surface layer, and wet- <br />ness. <br /> <br />5. Whakana-Porum <br /> <br />Gently sloping to moderately steep, moderately perme- <br />able to vel)' slowly permeable, loamy salls on uplands <br /> <br />This map unit consists of forested solis that have a <br />loamy surface layer and a loamy and clayey subsoil. <br />Slopes are 1 to 20 percent (fig. 4). This unit makes up <br />about 9 percent of the survey area It Is about 38 per- <br />cent Whakana soils, 15 percent Porilm solis, and 47 <br />percent other soils. <br />Whakana soils are gently sloping to moderately steep <br />and are on tops and sides of ridges of high terraces of <br />major streams. These solis are well drained and moder- <br />ately permeable. The surface layer Is brown, medium <br />acid fine sandy loam about 15 inches thick. Between <br />depths of 15 and 25 inches, the soil is red, very strongly <br />