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4 SOIL SURV brown, and brownish yellow clay. The underlying material 16 and 23 inches, the soil is yellowish brown, stron! is stratified, platy, and brownish yellow, light olive brown, acid loam that has strong brown mottles. Betwe and light olive gray shale to a depth of 80 inches, depths of 23 and 33 inches, the soil is yellowish bro~. Other soils are Ferris, Deport, Burleson, Austin, Ste- strongly acid clay lo. am that has rod and grayish, bro~ phen, Eddy, Trinity, and Elbon soils. Ferris, Deport, and mottles. Between depths of 33 and 44 inches, the'soil Burles0n soils are clayey, nearly level to strongly sloping light gray, very strongly acid clay loam that has dark r, soils on ridges and breaks. Austin, Stephen, and Eddy and yellowish brown mottles; uncoated sand and .~ soils are friable, gently sloping, silty clay on uplands grains are on vertical faces of pads. Between depths underlain by chalk. Trinity and Elbon soils are nearly 44 and 59 inches, the soil is light brownish gray, mediu level soils on flood plains, acibl clay that has dark red and yellowish brown mottle The soils in this unit are used mainly for crops and Between depths of 59 and 80 inches, the soil is lie pasture and hay. Many ponds and flood prevention struc- brownish gray, medium acid clay loam that has oli~ tures provide recreation. Some areas are covered with yellow, yellowish brown, and dark red mottles. urban works and structures, mainly residential. The soils Woodtell soils are sloping to strongly sloping and a: in this unit have high potential for crops, for range, and on sides of ridges. These soils are moderately wt for pasture and hay. Potential for woodland is Iow be- drained and very slowly permeable. The surface layer cause the soils are clayey and very slowly permeable, very dark grayish brown, slightly acid loam about There is no woodland grazing in this unit. inches thick. Between depths of 4 and 12 inches, t? The soils have Iow potential for urban development, soil is yellowish red, very strongly acid clay that has ligl The soils shrink and swell greatly with changes in mois- olive brown and light brownish gray mottles. Betwes turo content. They also are corrosive and have Iow depths of 12 and 26 inches, the soil is rod, very strong' strength. Potential for recreation is Iow because of very acid clay that has light brownish gray and light oliv slow permeability and the clayey surface layer, brown mottles. Between depths of 26 and 41 inches, th soil is mottled red and light gray, very strongly acid cia'. 2. Annona-Froestone-WOodtell Between depths of 41 and 51 inches, the soil is ligi Nearly/eve/to strongly slop/nE, slowlypermeab/e to very brownish gray, very strongly acid clay that has light ye slowly permeable, loamy $o#s on uplands Iowish brown and light olive brown mottles. Betwee depths of 51 and 63 inches, the soil is stratified grayis This map unit consists of forested soils that have a brown, partially weathered shale and clay that have ye loamy surface layer and a clayey subsoil. Slopes are 0 to Iowish brown mottles. 12 percent (fig. 2). This unit makes up about 23 percent Other soils are Derly, Hicota, Raino, Bernaldo, Guytor of the survey area. It is about 27 percent Annona soils, Ambia, and Roxton soils. Derly soils are Iqamy, poorl 19 percent Freestone soils, 11 percent Woodtell soils, drained, nearly level soils on terraces and ridgetop~ and 43 percent ether soils. Hicota and Raino soils are loamy soils on mounds withi~ Annona soils are gently sloping and are on tops and areas of Freestone and Derly soils. BernaIdo soils ar~ sides of ridges. These soils are somewhat poorly drained loamy, well drained, gently sloping soils on ridges and very slowly permeable. The surface layer is dark Guyton, Ambia, and Roxton soils are on frequent?. grayish brown, slightly acid loam about 4 inches thick, flooded bottom lands. Between depths of 4 and 9 inches, the soil is light The soils in this unit have medium potential for crops yellowish brown, strongly acid loam that has light grayish pasture and hay, and timber. Because of slope, wetness brown and brownish yellow mottles. Between depths of 9 and Iow fertility, nearly all of this unit is used for pastur~ and 16 inches, the soil is dark red, very strongly acid and hay or for timber. The gently sloping soils in this uni clay that has gray mottles. Between depths of 16 inches are suited to soybeans, corn, peanuts, truck crops, im 26 inches, the soil is light brownish gray, very strongly proved bermudagrass, clover, and tall fescue. Potentia acid clay that has dark red and gray mottles. Between for woodland grazing is medium because of Iow fertility depths of 26 and 42 inches, the soil is gray, strongly acid There is no range in this unit. clay that has dark red and yellowish brown mottles. Be- The soils in this unit have medium potential for mos tween depths of 42 and 55 inches, the soil is yellowish urban uses. The soils shrink and swell with changes ir brown, slightly acid clay that has gray and reddish brown moisture content. Other limiting features are slope, Io~ mottles. Between depths of 55 and 75 inches, the soil is strength, and wetness. Potential for recreation is mediun' mottled gray and yellowish brown, mildly alkaline clay. because of slope, slow or very slow permeability, an¢ Freestone soils are nearly level to gently sloping and wetness. are on ridges. These soils are moderately well drained and slowly permeable. The surface layer is brown, slight- 3. Wilson-Normangee-Crockett ly acid fine sandy loam about 6 inches thick. Between depths of 6 and 16 inches, the soil is light yellowish Nearly level to gently slop/nE, ve/y slowly permeable, brown, medium acid fine s~ndy loam. Between depths of loamy so#s on uplands