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' Typically, the surface layer is a pale brown to light brownish <br />gray loam 12 inches thick. The underlying material to a depth of 60 <br />' inches is very fine sandy loam or loam stratified with thin lenses of <br />sand, loamy sand, and clay loam. The soil is calcareous throughout. <br />' Permeability of this Haverson soil is moderate and available water <br />' capacity is high. The effective rooting depth is 60 inches or more. <br />Runoff is slow to medium, and the hazard of water erosion is slight. The <br />' hazard of soil blowing is moderate. <br />i ' Peetz gravelly sandy loam, 5 to 20 percent slopes. <br />' This deep, somewhat excessively drained soil is on backslopes and <br />shoulders of moderately dissected to highly dissected upland ridges and <br />' breaks. It formed in calcareous gravelly alluvium. Slopes are dissected <br />_ and convex. <br />Typically, the surface layer is grayish brown gravelly sandy loam <br />' 8 inches thick and is covered with 15 to 35 percent gravel and cobbles. <br />' The underlying material to a depth of 60 inches is calcareous very gravelly <br />sand. On steeper slopes this soil type combines into a rock outcrop com- <br />' plex. <br />' Permeability of this Peetz soil is moderately rapid to a depth of <br />8 inches and rapid below this depth. Available water capacity is moderate. <br />Effective rooting depth is 60 inches or more. Runoff is slow, and the <br />hazard of water erosion is slight to moderate. The hazard of soil blowing <br />t is slight. <br />1 <br />1 <br />1 <br />