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'+ k,fir; 114 -k 1 - <br /> _I�,�,,°'t '�I, r � ! <br /> :.71 lY r 'PI <br /> ` r ry S i .r.l._ aM'a 1 ..� •r 11 'r I•....x,�k 'a 11 L se <br /> n n f t I ^p .n hrj't <br /> Y.:�l "— P <br /> }rv4'4•I w •i�}.,+ief ,'jl� i,J:, <br /> 3b <br /> II <br /> In{u x,' I t1 x4 ! 1tI <br /> �rR h rlu , r <br /> I <br /> I` 'I}� k <br /> 111t1r 1'S �r !• I +, I. C� I,'�s:- I s t ' I I� '..�i I f ,� •,r{, Irl <br /> n.Fa, r#' Le r w a Tilt <br /> fn;5r IV- r' -=ra,!� ,! - 5 , ,4[� F'A"'++ti r t^ 'r. s' .�� s la ��i l• rr >ni,',1, SI 1 I�. I I- <br /> 11,p Slte;,Back `round;information �i <br /> b <br /> r "' lrl�lYi ,,4 I , 5' ,,; '� „FAST AND.EASY MART'S 1 '� <br /> i f i lh�l :, �• r. a s rt 1 { i'I , '' 1,- <br /> � ;' 244-West'Hardin Wa , Stockton;California tn�,.' f �•R ', +li ,Y 11 }t,; " ''' , <br /> gt .y <br /> I _r`� ^�s I,.I -; ij"_ PI • r� `• .'- r .. a s.,,II 14 1 F . . P n-3AB :,� I tll � <br /> II t I I 1s� ,r Ih Ih .�, �•'s Y t t,,. k. ; r , - .. i f ri r � , 17!� �y <br /> rll.•I , ^,I The szte'is.bounded onthe north by Harding Way,with resldenhal properties'orl the south and-west <br /> Ir1J 1A,y <br /> J I and,commercial properties'on'the east. A single'structure;utilized as a gasoline,station and'min>< r ray <br /> mart; occupies the'southein 1portioin of the site: Two underground .storage tanks (USts} <br /> .'., removed'from•the site in Septeriiber,l'99$by'Stockton�Service Station Equipment(SSSE)'and'anew I' _ <br /> � UST system was installed in December 1998. <br /> -i;.,REGIONAL'GEOLOGICIHYDROGEOLOGIC CONDI TIONS <br /> I, r <br /> The 'site'is situated within the Great Valley Geomorphic Province of California; a large, elongate <br /> „•• �', `'northwest-trending;'`asymmetric structural trough.,The Great Valley Province has been'filled withr' <br /> thick;sequerlces of.sedirnent ranging iri age.from Jurassic to'Recent,'creating,a nearly flat-lying' ' ^ <br /> ,'alluvial plain,which extends from the Tehachapi Mountains in the,south to the Klamath'Mountains : ". <br /> in the north The western and eastern boundaries.of this province are comprised of the-California <br /> CoastRange and the Sierra Nevada,'respectively., Rocks composing.the basement complex of the <br /> province have not been completely defined.but are believed to be of metamorphic-and igneous.'' <br /> ..origin.The Great Valley Province has been subdivided into two major divisions, identified as the <br /> ' Sacramento and San Joaquin Valleys. ; <br /> The Modesto, Riverbank; and Turlock Lake Formations and overlying Recent alluvium`are the . <br /> principal sources of domestic ground water in the 13;500-square mile San•Joaquin Valley Ground. <br /> Water:Basin (Basin 6-22). This basin is,drained primarily by the San Joaquin River.'The closest <br /> . <br /> r 'surface water featuie'at the site is Smith Canal and Yosemite Lake,located approxiinately'1,500:feet <br /> northwest of the:site. Water from Smith Canal drains into the San-Joaquin River'DeepWater"'. I} <br /> r .'r Anel and is rimaril .'used for commercial and-recreational boatin <br /> Cha p y g <br /> F I i ' ,; ,PREVIOUS INVESTIGATIONS ' <br /> '. '4 i ` , ' J ,... al srte,'assessment ., <br /> Itis Advanced GeoEnvironmental Inc. AGE s understanding that environment <br /> was performed on the property 'in early. 19,9,6. Field observations indicated that:petroleum <br /> ' hydrocarbons may have impacted the soil. 0 'e.;soil sample collected from 40 feet below surface} ; <br /> grade (bsg)had detectable concentrations of petroleum hydrocarbons. Two ground water,samples. <br /> `had low concentrations of volatile,aromatic compounds;one of the ground water samples'Collected ' <br /> ' a .`'•arid analyzed contained ,total• petroleum hydrocarbons, quantified as gasoline (TPH-g) 'at a <br /> r ;concentration of 0.28 milligrams per liter(mg/1).'Methyl'tertiary-butyl ether(MTBE)•was detected <br /> micrograms per liter(µg/1)• # <br /> Advanced GcoEnvironmenfal Inc. <br /> r:11 ' f � r .f � 5 , f '. tl rl Y .I rii•r <br />,r ,a.° � •: III � � " - � ' ,� � - l , ..,u c �'.� r � ,N ! I _'�a � �il ' <br />