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<br />' <br /> Exhibit B - Site Description <br /> <br /> Soils Information <br /> <br /> The soils for this area have been mapped and described by the U.S.D.A. <br />' <br /> Soil Conservation Service (SCS) in a published soil survey. This site <br />t consists of a single mapping unit: the Mesa Clay loam, 0 to 2 percent <br /> slopes. Figure B included herein is a soils map of the area delineating <br />' the mapping unit. A descriptions of the soil mapping unit is given below: <br /> MIA - Ptesa Clav Loam <br />1 S <br />il <br />f <br />M <br />d <br /> o <br />s o <br />the <br />esa series are deep, well drained, an <br />moderately fine <br />' textured. The soil occurs on high mesas and formed in gravelly or very <br /> gravelly alluvium of mixed mineralogy. Typically the surface layer is <br />' pinkish-gray or brown, granular, and about 3 to 4 i es thick. The <br /> subsoil is brown or light-brown clay loam that is about 8 inchethick. <br />' The s <br />bstr <br />\ <br />- <br />t <br />b <br />l <br />d <br />th <br />f 15 t <br />16 i <br />h <br />i <br />r b <br /> u <br />a <br />um, <br />ow a <br />er <br />y-pa <br />e <br />ep <br />o <br />o <br />nc <br />es, <br />s v <br />rown or <br />' brown loam that is calcareous and very gravelly and cobbly. Permeability <br /> is moderate and the available water capacity is fair. Atypical profile of <br />' the Mesa clay loam is attached. The Mesa clay loam, 0 to 2 percent slopes, <br /> are not highly susceptible to erosion. <br />1 <br />1 <br /> <br /> <br /> <br />-3- <br />