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Table 1-�S y�drologic Soil Groups for Soils in the Everett Area <br />S ' ('v <br />��. Alden�'ood <br />Hellingham <br />Cathcart <br />Custer <br />Eeoran <br />Indianola <br />Kitsap <br />L��nm�ood <br />McF�enna <br />I�Iukilteo <br />Norma <br />Pastik <br />Puget <br />Puyallup <br />Snohomisli <br />Sumus <br />'fokul <br />1\'inston <br />Hvdrolocic Soil Groun Classificntions <br />H��.irolocic Soil Grou� <br />C �� <br />C <br />C <br />C <br />a <br />A <br />C <br />A <br />D <br />D <br />D <br />C <br />C <br />B <br />D <br />C <br />C <br />A <br />A. Lo«• runoff potential. Soils ha��ine hig}, infiltration r tes, e��en ��hen thoroughl� <br />��etted, nnd consisting chiefly of deep, ��ell-to-excess ��•ely drained sands or <br />era��els. These soils ha��e a hieh rate oP��ater transmission. <br />B. `foderately lo�v runoff potential. Soils having moderute infiltration ntes u�hen <br />thoroughl} �eetted, and consistine chiefl�� of moderately fine to moderatel}' <br />coarse textures. These soils ha�•e a moderate rate of �� ater transmission. <br />—� C. �foderatelp hieh runoff potentiai. Soils ha��in¢ slow infiltration rates ��•hen �— <br />thoroughly� wetted, and consisting chieFl} of soils «•ith a layer Qiat impedes <br />do��mtard mo��emc:u of a�ater or soils ���ith moderately fine to finc teztures. <br />These soils hace a slo��� rate of ��ater trarumission. <br />D. High runoft potentinl. Soils ha��ing ven� slo�t• infiltrat on rates when ihoroughly <br />«etted and coisistine chiefly of cla� soil� ��ith a hieh s���elline potential, soils <br />with a permanent high �eatcr table, soils �eith a hardpan or clay laper at or near <br />the surface, and shallo��� soiL o�•er ncarly impen�ious ina+erial. These soils <br />ha� c a� en slo�v rate of ��ater transmission. <br />1-5•32 yc� <br />