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SECOR <br /> International Incorporated <br /> Logged By Date Drilled Drilling Contractor Project Name Method/Equipment Well Number <br /> Tosco 1205 <br /> TP 1116/02 CASCADE LATHROP,CA HOLLOW STEM AUGER MW-15 <br /> See"Legend to Logs"for Boring Surface Groundwater Depth(ft) Total Drive Drop <br /> sampling method, Dram(in) Elev(ft) V 15 FIRST Depth(ft) wt(lbs) Dist(in) <br /> classifications and laboratory 8„ 14.76(TOC) X 12 8 STATIC 250 140 30 <br /> testingmethods ( ) <br /> o <br /> Well Description <br /> Construction <br /> ro <br /> • CEMENT <br /> t GROUT <br /> SILTY SAND(SM),brown(7 5YR 4/2),dry,sand 80%fine 20%medium, <br /> BENTONI71 no petroleum odor,(0,70,30,0) <br /> 5 12 As above,medium dense 0 <br /> 7 <br /> #3 SAND 14 <br /> 2"DIA <br /> 0 020 <br /> SLO'T'TED <br /> SCREEN 10 12 As above 0 <br /> 11 <br /> 5 SAND(SP),grayish brown(10YR 5/2),dry,poorly graded,medium dense, <br /> sand 30%fine and 70%medium grained,no petroleum odor,(0,95,5,0) <br /> 15 16 As above 0 <br /> 16 CLAYEY SILT(ML),brown(7 5YR4/2),wet,hard,slow dilatancy,low <br /> 16 plasticity,no petroleum odor, (0,10,55,35) <br /> 20 <br /> 11 SILT w/clay(ML),brown(7 5YR4/2),saturated,very stiff,rapid dilatancy, 0 <br /> 15 non-plastic,no petroleum odor,(0,10,75,15) <br /> 15 <br /> THREADED SAND (SW),brown(7 5YR 4/3),well graded,loose,saturated,sand 35% <br /> END CAP fine 45%medium 20%course grained,no petroluem odor(0,90,10,0) <br /> The substrata descriptions above are generalized representations and based upon visuallmanual classification of cuttings and/or <br /> samples obtained during drilling Predominant material types shown on the log may contain different materials and the change from <br /> one predominant material type to another could be different than indicated Descriptions on this log apply only at the specific location <br /> at the time of dnlhng and may not be representative of subsurface conditions at other locations or tunes <br /> • Project No 77TO 43870.00 0222 Date 1124103 CH Log of Well <br /> 1205 GPJ Approved by <br /> LOG OF BOREHOLE Figure (sheet 1 of 2) <br />