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� — �,,._..-.. ,_. .. <br /> � Prclimin;iry Pindings from Revic�s� ofGcotcchnicil Rcports <br /> North Nlarina Dc��rlopmcnt <br /> � livcrctt, 1�'ashington <br /> �-tarch 24, 2004 <br /> CG Proje:t No. 157G <br /> I �'�l:c � <br /> 100 fcet before encuunt�rin� :i drnsc �uil la�cr. In gcner:il, thc dcpth to the drnse suil increases to the �ccst <br /> Ito�vards lhc channcl. <br /> IGroimdwalcr lilc�:uions <br /> 1Vc mc�surcd thc ground w-stcr cicvations thruugh a tidal cycic on January 3l, 2004, on dw sim at scvcn ground <br /> Iwatcr wclls installcd by Landau Associatcs. 'f}�ically, tid�l influcncc is not significant Qess than onc foot) 100 <br /> fect or more Gom the wat�r's edge. [3ccause of the nature of the fill and reportcd wood chips ar sawdust, it ���as <br /> Iconsidcred possible that marc influcncc could occur if channels of ntare pcmicable coarse matcrial existed within <br /> thc fill. Over lhe 8 hour tidal cycle which went from a high elcvation oC l 1.4 feet to a low elevation of 2.4 fect, wc <br /> Imcasured less than 0.2 fcet of maximum inllucnce in thc wclls. \Vhat we did find �vas an cllipticnl groundwater <br /> moimd in Ihc central portion of thc sitc. 7'hc long asis of thc moimd was in thc cast-wcst dircction. Thc maximum <br /> Ihcight of thc mound ���as mcasurcd at about cicvation 15 fcct �ti�ith thc lo��cst portion of Ihc mound at about 11? <br /> fccl. <br /> ITh� mound is consistcnt «iih uur �isunl obsenations at the site. 'l�he m�in acccs; ro:�d, 13t1i Street, essenti;illy, <br /> I bisects the site. On either side of this strect arc large svales that accept surtace storm ��•ater. Our interpretation is <br /> thnt these swalcs act as ground water infiltration areas and that the corresponding ground water mound is due to <br /> I a inrer storm water infiltration. \Ve expect this mound to bccome much less pronounced during Ihe dry summcr <br /> months. Measurements should bc taken thcn to verify this. \Vc would expect after dcvelopment that thc mound <br /> �vould essentially disappcar as surface infiltration should bc minimal. This ��•ould translate to a water icvcl of <br /> � abnut cic�ation I 1 fcct. �1'ith timc this cic�;itiun could bccumr somc�chat lo«cr�aithout ground ��atcr rcchargc. <br /> � PRI�.LI�IINARY UI�:SIG\ CONSIUGI2:�7'IONS <br /> Chc sienitcant gcotcchnical design considcrations arc as fallun s: <br /> " • The underlying soft silts will result in surficial settlement when subjected to ne��� loads. The building <br /> � loads �vould not cause significant settlement of thc lo���er soR silts, but could induce setUcmcnt in the <br /> upper soR soils. I.argc arcal fills should bc c�pccted to cause setdemcnt in the deeper suft soils, as «cll as <br /> in �he u��per soils. <br /> I <br /> � c <br /> Cornerstone Geotechnical, Inc. �/ � <br /> I <br />