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Unified Soil Classification System (USCS) <br />MAJOR DIVISIONS <br />SYMBOL <br />TYPICAL DESCRIPTION <br />Clean Gravels <br />GW <br />Well -graded gravels, gravels, gravel -sand mixtures, little or no fines <br />Gravels <br />(less than 5% <br />GP <br />(more than 50% <br />fines) <br />(j` <br />Poorly graded gravels, gravel -sand mixtures, little or no fines <br />of coarse fraction <br />GM <br />retained on No. 4 <br />Gravels with <br />Silty gravels, gravel -sand -silt mixtures <br />COARSE <br />sieve) <br />Fines <br />GC <br />Clayey gravels, gravel -sand -clay mixtures <br />GRAINED <br />(more than 12% <br />fines) <br />SOILS <br />(more than 50% <br />sw <br />retained on <br />Clean Sands <br />Well -graded sands, gravelly sands, little or no fines <br />No. 200 sieve) <br />Sands <br />(less than 5% <br />sP <br />(50% or more <br />fines) <br />Poorly graded sand, gravelly sands, little or no fines <br />of coarse fraction <br />passes the No. 4 <br />sieve) <br />Sands with <br />sM <br />Silty sands, sand silt mixtures <br />Fines <br />(more than 12% <br />SC <br />fines) <br />Clayey sands, sand -clay mixtures <br />ML <br />Inorganic silts of low to medium plasticity, sandy silts, gravelly silts, <br />or clayey silts with slight plasticity <br />Silts and Clays <br />(liquid limit less <br />Inorganic <br />OL <br />Inorganic clays of low to medium plasticity, gravelly clays, sandy clays <br />FINE GRAINED <br />than 50) <br />silty clays, lean clays <br />Organic <br />OL <br />Organic silts and organic silty clays of low plasticity <br />SOILS <br />(50% or more <br />passes the <br />MH <br />Inorganic silts, micaceous or diatomaceous fine sands or silty soils, <br />No. 200 sieve) <br />elastic silt <br />Silts and Clays <br />(liquid limit 50 or <br />Inorganic <br />CH <br />Inorganic clays of medium to high plasticity, sandy fat clay, <br />more) <br />or gravelly fat clay <br />Organic <br />OH <br />Organic clays of medium to high plasticity, organic silts <br />HIGHLY ORGANIC <br />Primarily organic matter, dark in color, <br />PT <br />Peat, humus, swamp soils with high organic content (ASTM D4427) <br />SOILS <br />and organic odor <br />1 Classification of Soil Constituents 1 <br />MAJOR constituents compose more than 50 percent, <br />by weight, of the soil. Major constituents are capitalized <br />(i.e., SAND). <br />Minor constituents compose 12 to 50 percent of the soil <br />and precede the major constituents (i.e., silty SAND). <br />Minor constituents preceded by "slightly" compose <br />5 to 12 percent of the soil (i.e., slightly silty SAND). <br />Trace constituents compose 0 to 5 percent of the soil <br />(i.e., slightly silty SAND, trace gravel). <br />Relative Density <br />(Coarse Grained Soils) <br />Consistency <br />(Fine Grained Soils) <br />N, SPT, <br />Relative <br />N, SPT, <br />Relative <br />Blows/FT <br />Density <br />Blows/FT <br />Consistency <br />0-4 <br />Very loose <br />Under 2 <br />Very soft <br />4 - 10 <br />Loose <br />2-4 <br />Soft <br />10 - 30 <br />Medium dense <br />4-8 <br />Medium stiff <br />30 - 50 <br />Dense <br />8 - 15 <br />Stiff <br />Over 50 <br />Very dense <br />15 - 30 <br />Very stiff <br />Over 30 <br />Hard <br />Cobalt Geosciences, LLC <br />P.O. Box 82243 <br />Kenmore, WA 98028 <br />(2o6) 331-1097 <br />www.cobaltgeo.com <br />cobalt eg o(&gmail.com <br />Grain Size Definitions <br />Description <br />Sieve Number and/or Size <br />Fines <br /><#200 (0.08 mm) <br />Sand <br />-Fine <br />#200 to #40 (0.08 to 0.4 mm) <br />-Medium <br />#40 to #10 (0.4 to 2 mm) <br />-Coarse <br />#10 to #4 (2 to 5 mm) <br />Gravel <br />-Fine <br />#4 to 3/4 inch (5 to 19 mm) <br />-Coarse <br />3/4 to 3 inches (19 to 76 mm) <br />Cobbles <br />3 to 12 inches (75 to 305 mm) <br />Boulders <br />>12 inches (305 mm) <br />1 Moisture Content Definitions 1 <br />Dry Absence of moisture, dusty, dry to the touch <br />Moist Damp but no visible water <br />Wet Visible free water, from below water table <br />Soil Classification Chart <br />Figure Ci <br />