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SECOR <br /> frirtrrsnHonallnco tired <br /> Luggcxl By Dat,.DnIkxl DnUn%Contractor E'n1)cct Nariic Mc.tlxxi/EgwIII tu.nt Bonin.Nwntxr <br /> Yrcci%ton Clie,,roti 9-2033 <br /> C Mclancun 8/30/00 Sampling 08 W Cliar-ter Way,Stockton,C Direct Pu%h SB- <br /> SM-Lege-Ild to I-og.- fur kaonnL Surface If" <br /> undwatcr Dcpili(ft) 1 otaI Driic Dnrlr <br /> vuurhng riuUk)d Ids sriL(ur) UUv(ft} y 45 5 1'tt tit Lncouritct cd ]7c I�th(ft ? �c t(Ib.) l�r't(rrs ) <br /> c4swlrcaUouti Out I ibuntcuy <br /> tc..�tur nxtlrc)(l. 2 Inch NA 20 St LbIh/cd 85 0 NA NA <br /> T <br /> � w <br /> S E)"Cllption <br /> Abandontinc.rrt � v <br /> .dSI -1 Y SAND(SM) Ntitth i la) Grcent,,h Gt�ty (101' 5/1) lint r ,uncal �snd 1 57 SIS 3 <br /> . ' dl.t]1l tnoi.l �lronw liychcx,<u bora odor (0 60 3n 10) (>>25 <br /> 4 a + <br /> ` v d <br /> ery ?06 5132 <br /> SILI Y CLA1' (CL) V tilt ftnc gtaincd sand Dark Gray(5� -t/l) -,cry•till C-,27 <br /> rnoi�l, medium pinqtcity moderate hydrex-arbon odor color changc-, to brown at i 17 <br /> 4 ' 29 no hydrocarbon odor (0 10 25 G5) <br /> s <br /> ap' 30 <br /> 16 SB-2 <br /> *vA As above-Olive Gray (5Y 42) Ca 30 <br /> •a`�A <br /> q r♦ <br /> •.a <br /> A <br /> ,^d T <br /> 5 <br /> . 'rid 35 SANDY SILT(ML) with clay. Darr Greenish Gray (10Y 4/1),fine grained <br /> :o'er sand,medium stiff, moist to wet (0,30,55,15) <br /> � a�r 1 <br /> SILTY CLAY (CL) with fine grained sand Dark Greenish Gray(10Y 4/1), <br /> i; very stiff,moist, medium.plasticity (0,15,30,55) <br /> t apt <br /> i� 40 <br /> die 2 SB-2 <br /> +;+� @40 <br /> �tAr <br /> a'�8 <br /> Nat, <br /> r As above-with uiterbedded silty sand stringers <br /> yr 45 <br /> F SAND (SP) with trace silt Dark Greenish Gray(10Y 311),fine grained sand, I <br /> V dense,wet (0,95,5,0) 18 SB-2 <br /> -ep @46 <br /> � (s <br /> Z d�r b <br /> �~ �rrfldCS to <br /> • — — — — — -- <br /> The substrata descriptions above axe generalized representations and based upon visual/manual classification of cuttings and/or samples <br /> obtained during drilling Predomuiarit matenal types shown on the log may contain different materials and the change from one <br /> predorrnnant matenal type to another could be different than indicated Descnptions on flus log apply only at the specific location it the <br /> time,of dnlling and may not be representative of subsurface conditions at other locations or times <br /> Pr0Jat No 077 4I991 017 Datc August 2000 Loi of Boring <br /> 92033 GPJ 1 Egurc <br /> LAC;Of 13ORFI iol-r <br /> (-,heel 2 cit 4) <br />