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t. e. _ ' i� <br /> �• ir "{ - ', ' ,.rr' �q .. '--"'� -,� - - <br /> s. or `q' �.y�'..�5' `. ' r r. °"rTr4 ,s,. �' , ',. r,.ra.."'1 3.y„� ;,i r. - (. <br /> t�.. ',� .: ::,ya�'iw 3F :•, ,s �,�- r:�y ?e. ''"•xr-a� - .�`: �`",- -w <br /> �,,. •'*t'Yc ,.,. r.,ar;z .r,.-,".,. ;.u"-. _.; -.:A'fi. .�-'�. XgAx.ir'?�". ,..y 7c 'r - .:i;. ',j,.. -7s %y,. {.'r'' ".-. ` "' . <br /> n -- `'k" `µ ' ' ,r'4 .,�' :.Y..- `C` _ <br /> '.y "Wn v,-.,•>+«.,.i,: :Y.r`"^._ 9 qya ,._' y 5. r,r; F�„"C xt„r„i.., +' ;...f ,yr`o ,,J,F-'� -, C�{ "i e,-�, xt: '� _ y ixrsX,� E ,y - r'' 5�i'^YA. -4,_.� ' <br /> :�.Ys.., rsx,�r_�r,�,��.., ,.,�= r- �;”? �� w,.�sy .sem,. � „7L>��.°Y:y � ":a•,�5�.�rs�`'=�g,;• v^r-a�.a�:�`;�r�- <br /> �yf <br /> . 6dS�jb <br /> .� 4.0 HYDROGEOLOGY <br /> The site as located within the central <br /> portion of the physiographic providence known as the Great <br /> I Valley, The Great Valley is a large elongate northwest-trznding asymmetric structural trough <br /> that has been filled with a thick sequence of sediments ranging in age from Jurassic to Recent. <br /> In the study area these sediments consist of a heterogeneous sequence of gravel, sand, silt, and <br /> clay deposited by the Sacramento River system. The sediments encou»tered during drilling <br /> consist primarily of an organic soil to approximately.S feet below grade underlain with peat to <br /> 12 feet. The soil beneath the peat consists of a fat clay to total depth of 15 feet below grade. <br /> Lithologic logs are presenwl in Appendix I. <br /> The deposits containing fresh groundwater in the area are principally unconsolidated continental <br /> deposits of Pliocene to Recent age that extend to depths ranging from lsss than ten to more than <br /> 3,500 feet. Groundwater was encountered during drilling activities at approx;mately 1.5 feet <br /> Mow grade. <br /> S•a FIELD INVESTIGATION <br /> € To Provide additional informaLon regarding subsurface conditions at the site, RESNA <br /> ! IndustrieslWaterWork Corp. supervised the drilling of 5 groundwater monitoring wells during <br /> the months of March and April 1991, The drilling was performed by ExcelTech Drilling of <br /> Fremont, California, utilizing a hollow-stem auger drill rig. The wells were situated to provide <br /> information regarding groundwater quality and hydraulic raulic conditions beneath the site(Figure 5), <br /> 5.1 Sampling Procedures <br /> All borings were sampled at approximately 1,0 to 2.5 feet below grade using a split-spoon <br /> sampler with brass Iiners. The brass liners were sealed at each end with aluminum foil and a <br /> plastic cap. The plastic cap was secured with tape and the sample placed on ice. The soil was <br /> logged by a qualified geologist using the Unified Soil Classification System. Descriptions of the <br /> soils encountered and monitoring well details were recorded on the,yell/boring logs(Appendix <br /> i <br /> Ii <br /> I j King Island Rmort-347 .. <br /> ! l Boe,s»,.WP 3 <br /> �J <br /> iiiiiii0l OWNS <br />