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<br />BI`_LINGS SILTY CLAY, MODERATELY DEEP OVER GREE1: RIVER SOIL MATERIAL, <br />0 t~ 2 percent slopes, Class IIIs Land (Be) <br />This soil occurs on the outer margin of coal•ascing alluvial fans <br />' where 1 to 4~ feet of fine-textured deposits derived from shale <br />overlies Creen River soil materials, <br />' E;:cept for a feu strips only a few rods wide that adjoin low-lying <br />areas of Green River soils, this soil has not been altered by high <br />' overflows from the Colorado River.. It is not likely that the main <br />part of the soil will be covered by floodwaters from the Colorado <br />Ri•rer, as it lies well above the level of normal overflow. <br />Drainage and saline conditions have to be corrected before the soil <br />will produce well. <br />t So;1 limitations are classified as severe for local roads and streets <br />(`:i,;h shrink-swell), dwellings with basements (high shrink-swell), <br />' d•.;1liugs without basements (high shrink-swell, cut banks cave), <br />sa-Mary land fill (cut banks cave), and septic tank absorption <br />fields (to about 40 inches, slow permeability). <br />1 <br />1 <br /> <br />.. <br /> <br />1 <br /> <br />