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APPENDIX A <br /> FIELD EXPLORATIONS <br /> SubsurFace conditions were explored at the site by drilling nine borings (B-1 through B-9) and excavating <br /> seventeen test pits (TP-1 to TP-17). Borings B-1 through B-5 were completed on April 8, 2009 to depths <br /> ranging from 18 feet to 281/2 feet below the existing ground surFace. Borings B-6 through B-9 where <br /> completed on March 3, 2014 to depths ranging from 8 feet to 201/2 feet below the existing ground <br /> surFace. Test pits TP-1 through TP-11 were completed on April 2, 2009 to depths ranging from 8 to <br /> 14 feet below the existing ground surface and TP-12 to TP-17 were compieted on April 24 and 25, 2014 <br /> to depths ranging from 4 to 8 feet. The locations of the explorations were estimated using a hand-held <br /> GPS device with sub-meter accuracy and by measuring distances from site features in the field by <br /> taping/pacing and should be considered approximate. The approximate locations of the explorations are <br /> shown on the Site Plan, Figure 2. Ground surface elevations shown on the exploration logs were <br /> estimated based on the base survey map shown on Figure 2. <br /> Borings <br /> The borings were completed using trailer-mounted, continuous-flight, hollow-stem auger drilling <br /> equipment, owned and operated by Geologic Drill Explorations, Inc. of Spokane, Washington. The borings <br /> were continuously monitored by a geotechnical engineer from our firm who examined and classified the <br /> soils encountered, obtained representative soil samples, observed groundwater conditions, and prepared <br /> a detailed log of each boring. <br /> The soils encountered in the borings were sampled at 21h to 5-foot vertical intervals with a 2-inch <br /> outside-diameter, split-barrel standard penetration test (SPT) sampler. The samples were obtained by <br /> driving the sampler 18 inches into the soil with a 140-pound automatic hammer free-falling 30 inches. <br /> The number of blows required for each 6 inches of penetration was recorded. The blow count("N-value") <br /> of the soil was calculated as the number of blows required for the final 12 inches of penetration. This <br /> resistance, or N-value, provides a measure of the relative density of granular soils and the relative <br /> consistency of cohesive soils. Where very dense soil conditions preclude driving the full 18 inches, the <br /> penetration resistance for the partial penetration was entered on the logs. The blow counts are shown on <br /> the boring logs at the respective sample depths. <br /> Soils encountered in the borings were visually classified in general accordance with the classification <br /> system described in Figure A-1. A key to the boring log symbols is also presented in Figure A-1. The logs <br /> of the borings are presented in Figures A-2 through A-10. The boring logs are based on our interpretation <br /> of the field and �aboratory data and indicate the various types of soils and groundwater conditions <br /> encountered. The logs also indicate the depths at which these soils or their characteristics change; <br /> although, the change may actually be gradual. If the change occurred between samples, it was <br /> interpreted. The densities noted on the boring logs are based on the blow count data obtained in the <br /> borings and judgment based on the conditions encountered. <br /> Observations of groundwater conditions were made during drilling. Groundwater conditions observed <br /> during drilling represent a short term condition and may or may not be representative of the long term <br /> groundwater conditions at the site. <br /> � <br /> GEOENGINEER� October24,2014 PageA-1 <br /> File No.0482-027-02 <br />