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�y <br /> • Groundwater <br /> zed at approximately 88 Feet deep in MW-1. <br /> Groundwater stabli <br /> dthree other wells located <br /> A survey wasofrun the between MWwaterlevels measured <br /> within 1,400' <br /> Ta of Well Elevation Water Level <br /> Well - <br /> 76.91 -6.38' <br /> MW-1 71.6 -4.44' <br /> 2,000 GPM well 68.47 -4.76' <br /> 5000 GPM Well 69.80 -6.30' <br /> office Well <br /> ' that gro�.indwater elevation in the 2,000 GPM <br /> Measurements indicate <br /> and the 504 GPM 11 is influenced by water pressures at a <br /> greater depth then in MW-1 and the office well• The shallow <br /> 1,000 <br /> water table slopes to �annotsbewetadeterminedt about 8fromfeettworwells. <br /> fees. <br /> The North south slop <br /> CONCLUSION <br /> Based on Borehole No. I and2thaand <br /> ththe <br /> confour contamination <br /> it <br /> excavations to 17 feet deep, appears <br /> is <br /> mostly in the upper 20 to 25 feet and directly below the tank <br /> hole. <br /> Borehole No. 1 indicates some contamination at 35 feet and <br /> 5 feet below <br /> l. The <br /> none 5 feet above or e course gravelsoils and <br /> between 29 feet deep and a feet are generally <br /> explainable reason for contamination at 35' <br /> sands. There's no <br /> ible this sample was contaminated during the <br /> feet deep. It's poss <br /> sampling process. <br /> The sample of groundwater indicates no contamination. <br /> The data indicates that the contaminated area is relatively <br /> small and is probably limited to an area about 25 X 25 X <br /> deep and has not contaminated the water table. <br /> 6 <br />