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wwrson seftakor, aim. -Uenswasmen eAoxoaoonp <br /> 2.2.2 Hydrogeologic Selling <br /> Subsurface investigations have been conducted at the Site from 1988 to present for the assessment <br /> of the lower and vertical extent of petroleum hydmcal"ns hgmriczlly released from former Site <br /> Opereftors. Soil beneath the She was coddled using hollow atom auger drill rigs and die lithulogy <br /> was described by a geologist haled on visual Observations. Boring lags were created for all 12 <br /> groundwater monitoring wells installed at the Site and from two deep soil borings (BH-13, and <br /> 1411-14). Soil bmings BH-1 through BB-12 were drilled to groundwater, ranging from 25 to 40 <br /> feet below ground surf (bgs), in Order to determine the extent of conmmbmtion prior to the <br /> excavation of impacted soil and were not Ingged For lithologic descriptions. <br /> Soil beneath the Silo is comprised of interconnected layers of sand, silt and day. "fhe Site is <br /> generally underlain by clay to a depth nfapproximately 14 feet bgs, silt to 18f tbgs and send to <br /> 48feet bgs. Silt and sand layerssepara d by clay ore located beneath the Site from 54 feet to 105 <br /> feet bgs. <br /> '1 h ve groundwater nines were encountered while drilling the deepest wall at the Site (MW-10). <br /> The shallow water table groundwater was is located in the upper wind layer. An intermediate <br /> water woe is located in a silt layer between 54 and 28 f bgs and is separated f the sand <br /> Loyd above by b-feet of clay. However the upper and intermediate groundwater zones ate <br /> contiguous at well MW-2 located down gradient from the Site. Me lower groundwater zone at <br /> MW-10 is located between 74 and 105 feet bgs and is separated from the Intermediate zone by 5 <br /> f of clay. The lower groundwater woe was not logged in boring Bill-14, htcatod 40f to the <br /> somhwest. The lower grouMwater zone appears to be semi-confined based on rising groundwater <br /> levels measured in the well shortly alter removing the well plug although the static water level in <br /> well MW-10 is similar to those in otter nearby wells. <br /> Groundwater elevations have historically ranged from approximately 25 reel bgs in 2011 to 50 <br /> ft in 1991. The initial wells (MW-I though MW-3) were installed in December 1988. Hermetic <br /> tine water bible subsequently dropped 15 feet and deeper Wells (MW4 through M W-S) were <br /> installed in August 1991. The water bible his rebounded 25 feet since I"I with small seasonal <br /> Budrrou0ns. <br />