Laserfiche WebLink
Its <br /> The Beverage Source 'Inc <br /> 202/7°9-5030 <br /> iy 25, 1988 <br /> gravels, sands and clay deposited by the Mckelumne River system. <br /> Barings drilled at the site encountered predominantly clayey and <br /> pebbly fine-to coarse grained sands. The generalized geologic <br /> cross sections (Figures 3 and 4) based on drill log data show the <br /> stratigraphic relations Of the clayey to silty sands and gravels <br /> which underlie the site. The multiple sand layers encountered <br /> during drilling coarsen with depth and appear to re laterally <br /> continuous across the site. <br /> first groundwater in ',the vicinity of the site is <br /> Depth to fir g <br /> 45 feet below /g=ade. Saturated sediments were <br /> appro.;a mately 35 to <br /> encountered�at approximately-�3§' eet below the surface during <br /> ,.; i � barin s at the site For this investigation. <br /> drilling of all g <br /> Groundwater monitoring performed at the site on April 4, an6 <br /> le r depths to grou.ndwate� or 38.41, <br /> April 21. 1988 revea_r_d average dip <br /> 38.08 and 37.53 feet in %,M-1, MW-2, and MEW-3, respectively. This <br /> data indicates an estimated g-oundwater flow direction to the <br /> southeast under a gradient of approximately 0.1 percent (see <br /> a ' _,ezometric Surface Maps) . Due to the rela . <br /> _ igtlr`'S ar� oT . the gre;.ad:aa:er gradient at the site, it is <br /> tively fla. :atu_oO <br /> foga'_ andLa SL.^J��� <br /> t3r�rsLii:lCd t0 .y_ =ea a , <br /> ycec wV file San cac t-1'"y :_,CCd Control ani <br /> i '3atiOn prCL � _ vvL_,� _ <br /> nfcr , <br /> -h-a =a' 1 Ox _9S . , t, <br /> ^.e eSLi- <br /> iYa�s= Cans?_'_"4at;cn Distri _ , as o= - <br /> ar `lo:'F d;reC.-cn is o rhe sCUZ :. <br />