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<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />.' <br /> <br />I <br /> <br />. <br /> <br />I <br /> <br />I <br /> <br />1'\ . . .....,... <br />!) J 'oj ,) ::.. .J <br /> <br />on fans and terraces are very strongly alkaline in reaction and high <br />in exchangeable sodium as evidenced by scattered "slick spots" that <br />are devoid of vegetation. Injurious accumulations of soluble salt <br />are largely restricted to bottomland soils and areas bordering shale <br />badlands. <br /> <br />The composition of this map unit by Great Soil Groups except for <br />Regosols that are included within Desert and Sierozem soils, is esti- <br />mated as follows~ <br /> <br />Percent <br /> <br />1949 Great Soil Group <br /> <br />1965 Great Group, Subgroup <br />or Family <br /> <br />Haplorthents <br />(Thin 45%) <br />(Lithic 10%) <br /> <br />55 <br /> <br />Lithoso1s <br />(Shale 45%) <br />(Sandstone lO%) <br /> <br />28 <br /> <br />Haplargids and Camborthids <br /> <br />Desert & Sierozem soils <br /> <br />7 <br /> <br />Alluvial soils <br /> <br />Haplorthents <br /> <br />5 <br /> <br />Solonetz soils <br /> <br />Natrargids <br /> <br />5 <br /> <br />Land types <br />(Shale badlands 5%) <br /> <br />Land types <br />(Shale badlands 5%) <br /> <br />The largest component of mapping unit 1 is shallow residual clay shale <br />soils on hills and ridges. Deeper soils occupy narrow gullied drainage- <br />ways and alluvial fans. They are forming in recent accumulations of <br />sediment washed from higher shale and sandstone hills. The deeper soils <br />on smoother slopes are productive at locations where irrigation water is <br />available. Deep soils are in many of the narrow valleys between Artesia <br />and Elk Springs. There are scattered tracts of irrigab1e land but many <br />individual areas are divided by deep channels and gullies. <br /> <br />Erosion in the rolling shale hills and shale badlands is spectacular <br />but is mainly geologic in nature. Deep and extensive gullying along <br />drainageways and narrow valleys is of much greater agricultural signi- <br />ficance. At many places dissection by gullies severely limits use of <br />the land. Bridging of gullies increases the cost of highway construction. <br /> <br />Soil Mapping Unit 2: Shallow, light colored loamy and rocky soils of <br />the deserts. <br /> <br />There is only one delineation of this unit on the map. It is mainly <br />confined to northwestern Rio Blanco County and very nearly surrounds <br />that segment of unit 1 adjacent to Range1y. It comprises l85,OOO acres <br />or about 8 percent of the Basin. <br /> <br />- l5 - <br />