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<br /> <br />• <br />16 SOIL SURVEY <br />than 60 inches. They are used for grazing, hay, and inches. They are used for grazing, hay, and irrigated <br />irrigated crops. <br />Representative profile of Glenberg fine sandy loam, <br />in an area of Glenberg-Haverson fine sandy looms, in <br />native grass, 1,200 feet north and 800 feet east of the <br />center of sec. 12, T. 19 S., R. 60 W. <br />Al-0 to 5 inches, light brownish-gray (lOYR 6/2) fine <br />sandy loam, dark grayish brown (lOYR 4/2) when <br />moist; weak, thin, platy structure; slightly hard, very <br />friable; nonsticky and nonplastic; calcareous; moder- <br />ately alkaline; abrupt, smooth boundary. <br />C-5 to 60 inches, pale-brown (lOYR 6/3) fine sandy loam <br />stratified with layers, less than 4 inches thick, of loamy <br />fine sand and silt loam, brown (lOYR 513) when moist; <br />massive; slightly hard, very friable; nonsticky and <br />nonplastic; calcareous; moderately alkaline. <br />[n places there are a few, One, distinct, strong-brown <br />(7.6YR 5/6, moist) mottles below a depth of 21 inches. The <br />Al horizon is fine sandy loam to loamy fine sand 4 to 12 <br />inches thick. The G horizon is mainly fine sandy loam thinly <br />stratified with loamy fine sand and loam. <br />Gh-Glenber -Hav - <br />p x is o ow erraces a ong a revers an tree s. t <br />is made up of about 60 percent Glenberg fine sandy <br />loam and 30 percent Haverson fine sandy loam. The <br />slope is 0 to 2 percent. Areas of this complex are <br />elongated and cover as much as 300 acres. The Glenberg <br />soil is near the stream, and the Haverson soil is away <br />from the stream. <br />The Glenberg soil in this complex has the profile de- <br />scribed as representative of the Glenberg series. The <br />Haverson soil has a profile similar to the one described <br />as representative of the Haverson series, but the sur- <br />face layer is fine sandy loam and the soil is redder. <br />Included with these soils in mapping are areas of <br />Las Animas soils that make up about 10 percent of the <br />acreage. <br />Runoff is slow, and the hazard of soil blowing is mod- <br />erate. These soils are subject to occasional, brief <br />flooding. <br />These soils have potential for nonirrigated pasture. <br />They are easily tilled. The native vegetation is western <br />wheatgrass, inland saltgrass, cottonwood, and tama- <br />risk. Capability units IIe-1, irrigated, and VIe-1, non- <br />irrigated; Sandy Bottomland range site. <br />Haverson Series <br />The Haverson series consists of deep, well-drained <br />soils. These soils formed on flood plains in loamy allu- <br />vium. The slope is 0 to 2 percent, and elevation is <br />4,300 to 4,800 feet. The average annual precipitation <br />is 12 inches. The average annual temperature is 53° F, <br />and the frost-free season is 145 to 175 days. The <br />native vegetation is mainly plains grasses. <br />In a representative profile the surface layer is light <br />brownish-gray silt loam about 6 inches thick. The <br />underlying material in the upper 9 inches is light <br />brownish-gray silt loam. Below that it is pale-brown <br />stratified silt loam, loam, and fine sandy loam that <br />extends to a depth of 60 inches or more. <br />Permeability is moderate, and the available water <br />capacity is high. These soils are moderately alkaline. <br />Their root zone extends to a depth of more than 60 <br />crops. <br />Representative profile of Haverson silt loam, in <br />native grass, 0.35 mile north and 0.05 mile east of the <br />southwest corner of sec. 4, T. 26 S., R. 60 W. <br />A-0 to 6 inches, light brownish-gray (lOYR 8/2) silt loam, <br />dark grayish brown (lOYR 4/2) when moist; weak, thin, <br />platy structnre parting W weak, fine, granular; soft, <br />friable; nonsticky and slightly plastic; calcareous; mod- <br />erately alkaline; abrupt, smooth boundary. <br />Cl-6 to 15 inches, light brownish-gray (lOYR 8/2) silt <br />loam, dark grayish brown (lOYR 4/2) when moist; <br />weak, medium, subangular blocky structure; slightly <br />herd, friable; nonsticky and slightly plastic; calcareous; <br />moderately alkaline; clear, smooth boundary. <br />C3-15 to 60 inches, pale-brown (lOYR 6/3) stxetifled silt <br />loam, loam, and fine sandy loam, brown (10YR 4/3) <br />when moist; massive; hard, friable; nonsticky and <br />slightly plastic; calcareous; moderately alkaline. <br />The A horizon is loam, silt loam, silty clay loam, or One <br />sandy loam 3 to 12 inches thick. The C horizon is stratified <br />silt loam, loam, fine sandy loam, and silty clay loam. <br />Ha-Haverson silt loam. This soil is on ]ow terraces <br />or bottoms of intermittent drainageways in the eastern <br />part of the survey area. The areas are elongated and <br />cover as much as 200 acres. <br />Included with this soil in mapping are small areas of <br />Glenberg and Bankard soils. <br />Runoff is slow, and the hazard of erosion is slight. <br />The soil is subject to frequent, very brief flooding. <br />This soil has potential for nonirrigated pasture. The <br />native vegetation is mainly western wheatgrass, blue <br />grams, alkali sacaton, and fourwing saltbush. Capa- <br />bility units IIw-1, irrigated, VIw-2, nonirrigated; <br />Saline Overflow range site. <br />Heldt Series <br />The Heldt series consists of deep, well-drained soils. <br />These soils formed on alluvial fans in clayey alluvium. <br />The slope is 2 to 6 percent, and elevation is 4,800 to <br />5,600 feet. The average annual precipitation is 12 <br />inches. The average annual temperature is 53° F, and <br />the frost-free season is 145 to 176 days. The native <br />vegetation is mainly short plains grasses. <br />In a representative profile the surface layer is light <br />brownish-gray silty clay loam about 3 inches thick. <br />The subsoil is light yellowish-brown silty clay about <br />11 inches thick.The underlying material is light yellow- <br />ish-brown silty clay about 9 inches thick over pale- <br />yellow silty clay that extends to a depth of 60 inches <br />or more. <br />Permeability is slow, and the available water capac- <br />ity is high. These soils are moderately alkaline. Their <br />root zone extends to a depth of 40 inches or more. They <br />are used for grazing. <br />Representative profile of Heldt silty clay loam, 2 to <br />6 percent slopes, in native grass, 0.3 mile east of the <br />west quarter corner of sec. 14, T. 20 S., R. 65 W. <br />A 1-0 to 3 inches, light brownish-gray (2.6Y 6/2) silty clay <br />loam, dark grayish brown (2bY 4/2) when moist; weak, <br />thin, platy structure parting to moderate, very fine, <br />granular; slightly hard, firm; sticky and plastic; cal- <br />careous; moderately alkaline; abrupt, smooth boundary. <br />BZ--3 to 14 inches, light yellowish-brown (2.bY 6/4) silty <br />clay, olive brown (2.6Y 4/4) when moist; moderate, <br />medium, prismatic atractare parting to moderate, medi- <br />