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eh <br />ESPEY, HUSTON &ASSOCIATES, INC. <br /> <br />Type Location: These sails are located neaz the center of Section 26, <br />T.155., R.85W, in Gunnison County, Colorado. <br />Range in Chazacteristics: Thickness of the mollic epipedon ranges from <br />7 to 15 inches, depth to calcazeous material ranges from 15 to 40 inches, <br />and thickness of the solum ranges from 20 to 50 inches. Organic carbon <br />in the mollic epipedon ranges from 0.8 to 2 percent and decreases <br />uniformly with increasing depth. The soil is 90 to 100 percent base <br />saturated. Cation exchange capacity ranges from approximately 60 to <br />90 milliequivalents per 100 grams of clay. Rock fragments range from <br />15 to 35 percent in a majority of the control section and aze mainly of <br />gravel size. <br />The Al horizon has hue of 2.5Y through 7.SYR, value of 4 or 5 dry, <br />2 or 3 moist and chroma of 1 or 2. It ranges from soft to slightly hazd. <br />• The B2t horizon has hue of 2.SY through 7.SYR, value of 5 or 6 dry, 3 <br />through 5 moist, and chroma of 2 through 4. It usually has prismatic to <br />subangulaz blocky structure but has angulaz blocky structure in some <br />pedons. The B2t horizon is gravelly heavy clay loam or light clay and has <br />35 to 50 percent clay. It is neutral or mildly alkaline. The Cca horizon <br />has hue of 2.SY through 7.SYR. It ranges from pH 8.0 to 8.6, and the <br />calcium cazbonate equivalent ranges from approximately 4 to 12 <br />percent. <br />Competing Series: These are the Arling, Brinkert, Brolliaz, Buckskin, <br />Florissant, Getta, Gothic, Gurney, Heath, Judy, Little Horn, Mayoworth, <br />Owen Creek, Segal, Sessions, Sneffels, Trout Creek, Waters and Youman <br />series. Arling soils have a significant component of volcanic ash and <br />other pyroclastics. Brinkert, Getta, Gothic and Youman soils lack <br />cazbonate above a depth of 40 inches and do not have ca horizons. <br />Brolliaz, Judy, Little Horn, Sneffels and Waters soils have a lithic <br />• <br />I-17 <br />