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Proposed Retail Dcvelopmeat J-1443 <br /> 112'�Street and Hwy.99 Febcuery 26,2004 <br /> CEvcrett;Washington Page 8 <br /> spalis and medium dense silty sand fill. Elsewh;re across the building pad, as well as below the <br /> fill soils and pcat, ihe borings encountered medium dense to very dense silty sand with some <br /> gravcl that was intcrproted to be weathered and unweathered glacial till. These soils were <br /> cncountered to the full depths explored. <br /> Parking.0.rcas,Outlots and 5tormwaler Managcment Area <br /> Soil conditions varied greatly in these areas. The topographically lugher portions of the <br /> main pazking area, as well as portions of Outlots #1 and #2 appeaz lo be underlain primarily by <br /> medium dense to dense silty sand to gravelly silty sand interpreted U� be glacial till. Elsewhere, <br /> one to 8 feet of soil intcrpreted to bc undo::umentcd fill was interpretcd to be prescnt above native <br /> soils that varied from soft peat to loose silty sand to very dense glacial till soils. <br /> The United Slates Departmen� of Agriculture Sor! 5urvey for Snohomish County, <br /> Washing�on (1983) indicates that the site is underlain by lhe Alderwood-Urban land complex. <br /> Alderwood soils are generatly described as glacially-derived gravelly sandy loam while Urban <br /> land is considered lo be covered with strcets, buildings, parking lots, and other stmctures that <br /> obscure or alter the soils so that identification is not feasible. Bascd on the results of our <br /> , evaluation,the majority of the site is considered to ba underlain by glacial titl soils that match thc <br /> descriptions of the Alderwood gravelly sandy loam. This soil is described by the USDA tc� have <br /> the following characteristics: <br /> � A(derwood gravelly sandy loam: <br /> • Low shrink-swell potential <br /> • pH range of 5.1 —6.5 <br /> • Permeability range of 2.0 to 6.0 in/hr in the upper 30 inches,negligible below 30 inches <br /> • Soil Hydrologic Group C <br /> • Slow runoff potential <br /> • Slight erosion hazard <br /> . Seasona] high perched groundwatcr betwccn 1% to 3 fcet below the gtound surFace between <br /> January and March <br /> • Low potential for frost action <br /> • Itisk of corrosion to uncoated steel and concrete is moderate <br /> • Unified Soil Classification Systcm classification of GM. <br /> Groundwater Conditions <br /> Slight to moderate groundwater sccpage was oUserved in 24 of the 32 borings completed <br /> as par[of this cvsluatioa. Additionally, slight lo heavy groundwater seepage was observed in 12 <br /> of the 21 tcst pits completed as part of this evaluation. The seepage observed was genetally <br /> interpreted to be perched groundwater abovc the dense to very dense glacial ti(1 soils. The depths <br /> to groundwater varied from I Y: to 9 feet below existing gades. Perched groundwater is likely to I <br /> bc more prevalent across the site during and after winter rains and aftcr winter rains and � <br /> / J-1443,022604 <br /> 8 � <br />