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<br />I <br /> <br />Most of the unit is at elevations between 7,000 and 8,000 feet but <br />there are extremes from 6,400 to 8,800 feet. Soil moisture conditions <br />are more favorable for plant growth due to higher precipitation and <br />lower evaporation associated with higher elevations. Data from the <br />Marvine station show a mean annual precipitation of about 20 inches, <br />a mean annual temperature of nearly 40. F., and a frost-free period <br />of 47 days. Since unit 5 extends west to the State line, a range <br />of from 15 to 20 inches in annual precipitation and 45 to 100 days <br />in length of frost-free period can be expected. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Parent materials consist of mixed alluvium, colluvium, and outwash <br />deposits along streams and valleys. Gravelly and stony valley fill <br />is extensive along the lower mountain slopes. Parent rocks are chiefly <br />sandstones, quartzites, shales and basalt. They have furnished the <br />source for much reworked material in which soils have formed. <br /> <br />I <br /> <br />I <br /> <br />The approximate composition of the unit by Great Soil Groups is shown <br />below. Estimates were not made for Regoso1s as they are included <br />within the zonal soils: <br /> <br />I <br /> <br />Percent 1949 Great Soil Group 1965 Great Group. Subgroup <br /> or Family <br />45 Chernozem soils Argiudolls and Argiborolls <br /> Hap1udolls and Hap10boro11s <br />35 Chestnut soils Argiusto11s and Hap1usto11s <br />15 Lithoso1s Hap1ustolls and Hap1udolls <br /> (Lithic) <br />3 Alluvial soils Hap1ustolls and Hap1a,!uolls <br />2 Land types Land types <br /> (Rock outcrop) (Rock outcrop) <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Dominant soils of this unit have dark gray or dark grayish brown <br />surface layers that are high in organic matter content. Surface <br />layers are loamy with loam and sandy loam textures being most common. <br />On steep colluvial slopes coarse fragments from higher lying rock <br />ledges and outcrops are usually scattered over the surface soil. <br />Subsoils are more clayey and may be sandy clay loam to clay in tex- <br />ture. Many subsoils contain gravel, stone, and rock fragments. Lime <br />is usually leached to depths of 40 to 60 inches. <br /> <br />I <br /> <br />Moderately deep and deep soils are intermingled within this unit. <br />At depths between 20 and 40 inches there is usually sandstone, shale <br />or basalt under moderately deep soils. Deep soils have formed in <br />valley fill and may have dark colored buried soils within the upper <br /> <br />I <br />I <br />I <br /> <br />- 22 - <br /> <br />I <br />I <br />