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fran neutral to mildly alkaline in reaction. The A horizon <br />ranges fran 16 to 40 inches in thiGmess. <br />Bg - Bangston fine sand, 1 to 10 percent slopes. This <br />soil is on hills and du*:ciike Lopography on uplands. <br />Included with this soil in mapping are a few small areas <br />of soils that have shale or sandstone at a depth of 40 to 60 <br />inches, small areas of soils that have slopes of as much as 25 <br />percent, and small areas of a nearly level fine sandy loam on <br />terraces. <br />Runoff is slow. The hazard of soil blowing is severe, and <br />the hazard of water erosion is moderate. <br />Most of the acreage of this soil is in native grass and <br />is used for grazing. A small acreage is irrigated and used for <br />grass hay and pasture. If this soil is irrigated, an organic <br />mat 1 to 4 inches thick generally forms on the surface and bright, <br />rust-colored mottles form throughout the profile. Capability <br />units VIe-5, non-irrigated, and VIe-10, irrigated; Sandy Bench <br />• range site. <br />TINE SERIES <br />The Tine series consists of deep, well drained soils that <br />formed in coarse textured alluvium. The soils are underlain by <br />gravelly loamy sand at a depth of 15 to 25 inches. They are on <br />terraces and outwash plains between elevations of 7,900 and 8,400 <br />feet. Slopes are 2 to 5 percent. The native vegetation is mainly <br />needleandthread, pine needlegrass, muttongrass, blue grama, sheep <br />fescue, streambank wheatgrass, Sandberg bluegrass, bitterbrush, <br />and big sagebrush. The mean annual precipitation is 12 to 15 <br />inches, the mean annual air temperature is 36° to 38° F, and the <br />frost-free season is 35 to 40 days. <br />yer is brown sandy <br />loam about 12 inches thick. The upper part of the underlying <br />material is brown loamy fine sand about 6 inches thick, and the <br />lower part, to a depth of about 60 inches, is brown gravelly loamy <br />sand. <br />Permeability is rapid, and available water capacity is <br />low. <br />E-2 <br />