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SECOR 0 <br /> Intem clonal Incorporated <br /> Logged By: Date Drilled: Drilling Contractor Project Name: Method/Equipmenc Well Number: <br /> CASCADE CHEVRON 20-0764 HOLLOW STEM AUGER <br /> EG 10/15/01 DRILLING STOCKTON,CA SPLIT SPOON MW-2 <br /> See"Legend to Logs"for Boring Surface Groundwater Elevation(ft.): Total Drive Drop <br /> sampling method, Dian(in.): Elev.(fr.): -7 -41.75 FIRST Depth(ft): wt.(lbs.): Dist.(ia): <br /> classifications and laboratory 8 18.25 70.0 140 30 <br /> testin methods <br /> e a <br /> Well 3 Description <br /> Construction <br /> A <br /> h <br /> BENTONM 14 SILTY CLAYEY SAND(SM): strong brown(7.5YR4/6), 0 MW2 <br /> SEAL 15 fine-grained sand,medium dense,slightly moist,no odor(0,55,25,15). @50' <br /> 17 <br /> r SAND <br /> 0.020" <br /> SLOTTED 55 15 SAND with CLAY(SC):brown(7.5YR4/4),fine-grained sand with 0 MW2 <br /> SEEN 15 some medium-grained sand,medium dense,slightly moist,no odor @55' <br /> CR <br /> 17 (0,85,5,10). <br /> 60 15 Encountered water. 0 MW2 <br /> 15 @60 <br /> 17 <br /> 65 12 SAND(SP):brown(7.5YR4/4),fine-grained sand,medium dense, 0 MW2 <br /> 13 wet,no odor(0,95,5,0). @65' <br /> 15 <br /> THREADED 70 SAND(SW):fine-to coarse-grained sand,well graded,loose,wet,no <br /> END CAP 15 odor(0,100,0,0). 0 MW2 <br /> 15 @70' <br /> 15 <br /> The substrata descriptions above are generalized representations and based upon visual/manual 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 drilling and may not be representative of subsurface conditi ovations or times. <br /> O` <br /> Project No. 77CH.43585.00.0203bate 10/27/01 PR � uCOTT � Log of Well <br /> lu GABLE ' <br /> 764MW2.GPJ s No. 636 '{ APProvedby <br /> LOG OF BOREHOLE tp ' <br /> ;-k Exp. `Q Figure (sheet 3 of 3) <br /> 0F CAS\F� <br />