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American Property DevelL, .ient ES-0599.05 <br /> January 16, 2015 Page 3 <br /> Updated January 22, 2015 <br /> At the boring locations, native soils consisting predominantly of medium dense to very dense <br /> silty sand with small amounts of gravel (21 to 4 percent) were encountered. These soils are <br /> classified by the Unified Soil Classification System as silty sand with gravel (SM). At both <br /> borings dense silty sand deposits were encountered the entire length of the boring. The only <br /> significant change in lithology was at boring B-1 where the upper twenty feet of samples were <br /> 21.1 percent gravel. This was the highest percentage of gravel content for the site. However, <br /> below twenty feet gravel percentage deceases significantly. The lower gravel content (3.8 to <br /> 13.3 percent) is characteristic of the subject property. Overall the soils at both borings appear <br /> to be similar in sorting and silt content. In general, test pits recently excavated confirm these <br /> conditions. <br /> The geologic map of the area identifies Quaternary Till (Qqt) deposits throughout the site and <br /> surrounding areas with is consistent with the results of the soil borings. With respect to the <br /> subject property, we interpret the upper dense to very dense deposits of silty sand with gravel <br /> to be associated with Quaternary Till. <br /> In general, the dense to very dense silty sand with gravel and sand deposits exhibit relatively <br /> good soil strength characteristics. In our opinion, the erosion potential of these soils can <br /> generally be characterized as low to moderate. <br /> Groundwater <br /> Groundwater was not encountered at the test locations. However, locally perched groundwater <br /> seepage is possible during the construction phase of the project. Groundwater seepage can <br /> generally be characterized as a perched condition at the contact between the upper deposits of <br /> fill and weathered native soils, and the underlying unweathered glacial till deposits. Due to the <br /> anticipated depth of the proposed garage level excavation, we anticipate perched groundwater <br /> seepage will be encountered in the proposed excavations. Due to the generally dense to very <br /> dense condition of the native soils, we do not anticipate groundwater seepage will adversely <br /> impact excavation stability, provided the excavations are appropriately sloped or shored. <br /> It should be noted that groundwater seepage rates and elevations fluctuate depending on many <br /> factors, including precipitation duration and intensity, the time of year, and soil conditions. In <br /> general, groundwater seepage rates and levels are generally higher during the wetter, winter <br /> months. <br /> Geologcally Hazardous Areas and Environmental Sensitive Features Review <br /> As part of our report preparation, we reviewed available maps and resources to identify <br /> designated geological hazardous areas for the site. Specifically, we reviewed the city of <br /> Everett's municipal code regarding Environmental Sensitive Features (37.40) and Geological <br /> Hazardous Areas (37.080). <br /> Earth Solutions NW,LLC <br />