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SECOR <br /> I/0-1440-al /rF2rporated <br /> lLot,�-cd By Dot, Diiii,a Dnllat-(,heir tir I'm]Lcct NtuIx N'tL01tW-Malwl,l1 it( Bmtig Nwtdw <br /> Precnl<rli Ciic%[on 9 2011 <br /> OIC Niel tiuuli H/1{M/0() S,Inil>hni 08 1t' Charter \'Vey,St(pcktmi, (: 1)[[cct Pw ll SB-2 <br /> Sex 1 c�utJ tai l�,r. lir 13 ,nils Surrto ( muiid%yMtr I)Ll)ih(Il ) 11)uI l?rnt I�n,h <br /> `ampling iitttltud I�I�nt U % (It) SZ 45 5 I [[�f l:ncuuntcr cd IN hilt(I I ) ,�I(Il). ) IJ1`f(lit <br /> als ) <br /> vihcatatin..Uld I+h�rrtSit) <br /> lCZ,U11 A mhlik,dN 2-Inch NA Z 20 Slebdtied 85 0 NA NA <br /> L <br /> Iiol Inti u v _ <br /> U y C <br /> -� � l�c,ull)flc)II y 2 v <br /> Ah indomm nl J ❑ Lw <br /> ❑ V 9 <br /> o c O <br /> P <br /> a ao 0 511,11' tiAjNl) (5111) I 11-1, Nsith �,i nd end (i dcc cl t% BIOMI(10)'1' 413) Ilnc <br /> 'd a er<uiu.d .,end l uyt-grdint,d gidvd d1121.11,u hlUl. I l uli, moll inulllcd.Ihln ar utc t <br /> p ry (1065205) <br /> �* a <br /> 00 <br /> ~� pD <br /> � o r <br /> �a�d BdcklillLd S 4 <br /> o Q . with Ce[rient <br /> Grout <br /> R • <br /> � r <br /> •.a t <br /> s d <br /> 10 As above-no gravel,uniform structure indicates native <br /> T •P <br /> • d� <br /> ��Or <br /> r SILTY CLAY(CL) with fine grained sand Dark Grayish Brown(10YR 42), 0 SB-2 <br /> tea: 15very stiff,moist,medium plasticity (0,10,25,65) @14 <br /> y ,�a <br /> � r <br /> i t• <br /> ;0..•.r <br /> SANDY SILT(MI.)with clay.Dark Greciush Gray(l0Y 4/1),fine grained <br /> sand,very stiff.moist,low plasticity (0,35,55,10) <br /> yr�Ir A <br /> « E 20 <br /> �+ * Grades to _ 4 SB-2 <br /> y � SILTY CLAY(CL) with trace fine grained sand Dark CnreriuhGray(SGYJ 920 <br /> <<4 4/1),stiff,moist,medium plasticity,moderate hydrocarbon odor (0,5,40,55) <br /> 4 <br /> R <br /> w <br /> •r 33 <br /> The substrata descriptions above are generalized repre-tntations and based upon visual/manual classification of cuttings and/or earnples <br /> obtained duruig dnllmg Predominant material types shown on the log may contain different matenals and the change from one <br /> predominant mate-nal type to another could be different than indicated Descriptions on flue log apply only at the specific location dl the <br /> time of drilling and may not be representative of subsurface conditions at other location,or times <br /> Prnlocl No 077 41991 017 Datc August 2000 Log of Bormig <br /> 92033 GI! <br /> LUOQ OI'BOR UiOLI_ <br /> (Nh(-,c,t I of 4) <br />