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GeoTesl Services,Inc. June 3, 2005 <br /> Baldwin Residence,3206 Wave Dnve, Evereri,WA Job No. 5233 <br /> Site Soil and Groundwater Conditions <br /> GeoTest Services, Inc. conducled iimiled site explorations during the time of our visit. <br /> Our subsurface explorations consisted of three Dynamic Cone Penetrometer (DCP) <br /> tests in order to help evaluate the subsurface soil densities within the existing wall <br /> locations and the proposed upper wall location. A DCP probe includes recording the <br /> number of blows necessary to advance a pointed steel rod into the ground with a 35- <br /> pound drop hammer. Thie blows necessary to advance the rod into the soil have been <br /> correlaled with the density of granular soil deposits and the consistency of cohesive <br /> soils. The ihree DCP tests were conducted along the middie bench poriion of the <br /> existing wall system. The three DCP tests were conducted to maximum exploration <br /> depths of 4 feet 8 inches, 6 feet and 3 feet 4 inches at DCP-1, DCP-2 and DCP3, <br /> respectively. A distinct change in density was observed in all three test locations. At <br /> DCP-1 and DCP-2 the contact was interpreted to be between loose, possible previous fill <br /> soils, and more compe!ent native soils at a depth oi 4 feet below existing ground surface <br /> (BGS) and 3 feet 4 inches at the two locatioiis. The change in density observed at <br /> approximately 1 feet 4 inches BGS in DCP-3 was interp �:ted to be between the upper <br /> more loose native slope soils and the underlying more competent undisturbed native <br /> soils. Logs of the DCP analysis are included in the appendices of this report. A�ao refer <br /> to the Site and Explorafion Plan, Figure 2, for more detail regarding exploration <br /> lucations. <br /> Observed soils within the unfinished wall section appeared to be native cut areas <br /> consisting of moisl, light brown siltylclayey sand with gravel and trace cobble or boulder. <br /> The undisturbed native soils were medium dense to dense and appeared consistent v. th <br /> glacial till mapped in the area of the property. We understand that some pravious fill <br /> soils andlor debris may also have been present within the northern portion of the existing <br /> wail locations. We are unsure if all of the potential previous fill soils or debris was <br /> removed prior to the construction of the originai H all system. <br /> Groundwater seepage was not encountered within any uf the explorations conducted <br /> during our site visit. We would expect that a regional groundwater level would not be <br /> encountered within the scope of this project. However, incident stormwater runoff <br /> perched at the contact of looser near sur(ace soils or within previous fill soils and the <br /> denser till-like soils may be encoun;ered depending on the time of excavation. <br /> Groundwater seepage may be expected to emanale trom sandier zones within the <br /> native soils, as well as from random locations in existing fill soils, and at the contact <br /> between fill and underlying native soils. Groundwater levels are not static and vary with <br /> respect to surface runoft, precipitalion, season, changes in sile utilization, both on and <br /> off site, and othEr factors. <br /> Tlie retaining wall design recommendations provided herein are based on the findings of <br /> our limited site exploralions. Accordingly, we recommend that competent personnel <br /> monitor construction of lhe retaining walls and that contingencies for differing site <br /> condilions be incorporaled into the project contract documenls lo aliow for necessary <br /> changes in design and cons!ruction methods. <br /> , <br /> Page2of7 �i , � <br />