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74 Soil Survey <br /> producing woody shrubs at a level that decreases the water capacity is very low. The shrink-swell potential is <br /> extent of the preferred forage plants. high. The effective rooting depth is limited by the <br /> This map unit is in capability subclass Vie bedrock at a depth of 10 to 20 inches. Runoff is very <br /> (MLRA-15), nonirrigated. The uneroded and eroded rapid, and the hazard of water erosion is very severe. <br /> Honker soils are in vegetative soil group D, and the The eroded Honker soil is moderately deep and well <br /> Vallecitos soil is in vegetative soil group G. drained. It formed in material weathered from <br /> sandstone. Typically, the surface layer is light brownish <br /> 178—Honker-Vallecitos-Honker, eroded, complex, gray gravelly loam about 7 inches thick. The upper 11 <br /> 50 to 75 percent slopes. These very steep soils are on inches of the subsoil is light brown gravelly clay loam. <br /> dominantly south-facing slopes on mountains. The The lower 13 inches is a claypan of light red gravelly <br /> native vegetation is mainly annual grasses, forbs, and clay. Hard sandstone bedrock is at a depth of 31 <br /> chaparral. Elevation is 800 to 3,300 feet. The average inches. In some areas the surface layer is gravelly clay <br /> annual precipitation is 12 to 18 inches, the average loam. <br /> annual air temperature is about 60 degrees F, and the Permeability is very slow in the eroded Honker soil. <br /> average frost-free period is 220 to 240 days. Available water capacity is low. The shrink-swell <br /> This unit is 35 percent Honker loam, 30 percent potential is high. The effective rooting depth is limited <br /> Vallecitos gravelly loam, and 20 percent Honker by the bedrock at a depth of 20 to 40 inches. Roots are <br /> gravelly loam, eroded. The components of this unit restricted to cracks and the faces of peds in the <br /> occur as areas so intricately intermingled that it was not claypan, which is at a depth of 8 to 16 inches. Runoff is <br /> practical to map them separately at the scale used. very rapid, and the hazard of water erosion is very <br /> Included in this unit are small areas of Honker and severe. <br /> Vallecitos soils that have slopes of more than 75 or less This unit is used for livestock grazing or wildlife <br /> than 50 percent and small areas of Gonzaga and habitat. General management considerations include <br /> Franciscan soils. All of these included soils are in the very severe hazard of erosion, the slope, the very <br /> landscape positions similar to those of the dominant low or low available water capacity, the limited depth of <br /> Honker and Vallecitos soils. Also included are small the Vallecitos soil, and dense stands of chaparral in <br /> areas of exposed bedrock in convex positions near the moderately eroded areas. The characteristic plant <br /> top of the slopes. Included areas make up about 15 community on the uneroded Honker and Vallecitos soils <br /> percent of the total acreage. is mainly soft chess, wild oat, and filaree. That on the <br /> The uneroded Honker soil is moderately deep and eroded Honker soil is mainly soft chess, red brome, and <br /> well drained. It formed in material weathered from California sagebrush. Grazing should be controlled so <br /> sandstone. Typically, the surface layer is brown loam that desirable vegetation, such as soft chess, is <br /> about 5 inches thick. The subsoil is a claypan of brown maintained and enough vegetation is left standing to <br /> and strong brown gravelly clay about 28 inches thick. protect the soils from erosion. Loss of the surface layer <br /> Hard sandstone bedrock is at a depth of 33 inches. In results in a severe decrease in productivity and in the <br /> some areas the surface layer is clay loam, gravelly clay potential of the unit to produce plants suitable for <br /> loam, or gravelly loam. grazing. The very steep topography and the resulting <br /> Permeability is very slow in the uneroded Honker runoff reduce the amount of rainfall that enters the soils. <br /> soil. Available water capacity is low. The shrink-swell The slope limits access by livestock and results in <br /> potential is high. The effective rooting depth is limited overgrazing of the less sloping areas. The very low or <br /> by the bedrock at a depth of 20 to 40 inches. Roots are low available water capacity limits the production of <br /> restricted to cracks and the faces of peds in the desirable forage plants. Fencing is difficult because of <br /> claypan, which is at a depth of 10 to 20 inches. Runoff the depth to bedrock. Brush management improves <br /> is very rapid, and the hazard of water erosion is very areas of range that are producing woody shrubs at a <br /> severe. level that decreases the extent of the preferred forage <br /> The Vallecitos soil is shallow and well drained. It plants. <br /> formed in material weathered from sandstone. Typically, This map unit is in capability subclass Vile <br /> the surface layer is pale brown gravelly loam about 4 (MLRA-15), nonirrigated. The uneroded and eroded <br /> inches thick. The subsoil is pale brown and brown Honker soils are in vegetative soil group D, and the <br /> gravelly clay loam about 16 inches thick. Hard Vallecitos soil is in vegetative soil group G. <br /> sandstone bedrock is at a depth of 20 inches. In some <br /> areas the surface layer is loam, gravelly clay loam, or 179—Itano silty clay loam, partially drained, 0 to 2 <br /> clay loam. percent slopes. This very deep, poorly drained, nearly <br /> Permeability is slow in the Vallecitos soil. Available level soil is on flood plains and deltas. It formed in <br />