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MESA COUNTY AREA, COLORADO <br />Youngston Series <br />The Youngston series consists of deep, well-drained <br />soils. These soils formed in alluvium on flood plains <br />and alluvial fans. The slope is 0 to 3 percent, and ele- <br />vation is 4,800 to 5,400 feet. The natural vegetation is <br />mainly saltbush, rabbitbrush, galleta, and Indian rice- <br />grass. The average annual precipitation is 9 inches. <br />The mean annual temperature is 520 F., and the frost- <br />free season is 160 to 175 days. <br />In a representative profile the surface layer is light- <br />gray loam about 4 inches thick. The underlying layers <br />are light brownish-gray sandy loam, very pale brown <br />loam, and pale-brown very fine sandy loam and loam <br />that extend to a depth of 60 inches or more. <br />. Youngston soils have moderate permeability and a <br />high available water capacity. They are moderately al- <br />kaline. Roots can penetrate to a depth of more than 60 <br />inches. <br />These soils are used for grazing, as wildlife habitat, <br />and as watershed areas. <br />Representative profile of Youngston loam, NWl/4 <br />sec. 9, T. 2 N., R. 2 W., in an area of grass. <br />A1-0 to 4 inches, li ht -gray (10YR 7/2) loam, dark gray- <br />ish brown flOYR 4/2) moist; weak, thin, platy <br />parting to weak, fine, granular structure; soft, <br />very friable; calcareous; moderately alkaline; <br />clear, smooth boundary. <br />AC-4 to 8 inches, light brownish-gray (10YR 6/2) sandy <br />loam, dark grayish brown (10YR 4/2) when <br />moist; weak, thin, platy parting to weak, fine, <br />granular structure; loose, very friable; calcare- <br />ous; clear, smooth boundary. <br />CI-8 to 20 inches, very pale brown (10YR 7/3) loam, <br />brown (10YR 5/3) when moist; weak, fine, sub- <br />angular blocky parting to weak, fine, granular <br />structure • slightly hard, friable, calcareous; mod- <br />erately alkaline; clear, smooth boundary. <br />C2-20 to 38 inches, pale-brown (10YR 6/3) very fine <br />sandy loam, dark brown (10YR 4/3) when moist; <br />weak, fine, subangular blocky parting to weak, fine, <br />granular structure; slightly hard, friable; calcar- <br />C3-38 to 60 nchesa pale brown ;(10YR 6/3)t loam, l dark <br />brown (10TR 4/3) when moist; massive- hard <br />when dry, very friable when moist; calcareous; <br />moderately alkaline. <br />The Al is loam or very fine sandy loam. Coarse frag- <br />ments make up as much as 15 percent, by volume, but com- <br />monly less than 5 percent of the soil. <br />Yo-Youngston loam. This soil is nearly level and <br />is on flood plains and alluvial fans. It has the profile <br />described as representative of the series. <br />Included with this soil in mapping are areas of <br />Billings soils. <br />. Runoff is slow to moderate. The hazard of erosion is <br />moderate. <br />This soil is used mainly for grazing and as wildlife <br />habitat. Capability unit VIe-1; Loamy Salt Desert <br />range site. <br />Use and Management of the Soils <br />The soils in the Mesa County Area are used mainly <br />for range. A small acreage is used for irrigated pas- <br />ture, hay, and crops. This section discusses these uses <br />and the suitability of the soils for roads, farm ponds, <br />and other engineering structures. It also provides in- <br />21 <br />formation on managing the soils for several land uses <br />and for wildlife habitat. <br />Crops, Hay, and Pasture <br />The small acreage used for irrigated crops, hay, and <br />pasture makes up less than 0.1 percent of the Mesa <br />County Area. The main crops are barley, oats, and <br />corn. Pasture and hay plantings are mainly alfalfa or <br />a mixture of alfalfa or clover and brome or fescue <br />grasses. <br />Estimated yields of crops are given in the discussion <br />of individual capability units on the following pages. <br />The range of yields given are those that can be ex- <br />pected from a reasonably high level of management <br />which includes the :following: <br />1. Using cropping systems that maintain good <br />tilth and a high content of organic matter. <br />2. Controlling erosion to the maximum extent <br />feasible, so that the quality of the soil is main- <br />tained or improved. <br />3. Maintaining; a high level of fertility by using <br />fertilizer ir.' amounts recommended by the <br />Colorado Agricultural Experiment Station. <br />4. Using crop residues to the fullest extent prac- <br />ticable to protect and improve the soil. <br />5. Following minimum tillage practices to re- <br />duce soil compaction and erosion. <br />6. Using adapted crop varieties. <br />7. Controlling weeds by tillage. <br />Capability Grouping <br />Capability groupin;? shows, in a general way, the <br />soiuitability of soils fo:r most kinds of field crops. The <br />sls are grouped according to their limitations when <br />used for field crops, the risk of damage when they are <br />used, and the way they respond to treatment. The <br />grouping does not take into account major and gen- <br />erally expensive landforming that would change slope, <br />depth, or other characteristics of the soils; does not <br />take into consideration, possible but unlikely major rec- <br />lamation projects; and, does not apply to horticultural <br />crops or other crops requiring special management. <br />Those familiar with the capability classification can <br />infer from it much about the behavior of soils when <br />used for other purposes, but this classification is not a <br />substitute for interpretations designed to show suit- <br />ability and limitations of groups of soils for range or <br />engineering. <br />In the capability system, the kinds of soil are <br />grouped at three levels : the capability class, the sub- <br />class, and the unit. These are discussed in the follow- <br />ing paragraphs. <br />CAPABILITY CLASSES, the broadest groups, are des- <br />ignated by Roman numerals I through VIII. The nu- <br />merals indicate progressively greater limitations and <br />narrower choices for practical use, defined as follows : <br />Class I soils have few limitations that restrict <br />their use. i <br />Class II soils have moderate limitations that re- <br />duce the choice of plants or that require mod- <br />erate conservation practices. <br />Class III soils have severe limitations that reduce