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r5 <br /> t <br /> • Table 1 Groundwater Monitoring Well Data <br /> Well No Date Well Depth to Casing Water Floating <br /> Depth (ft) Water (ft) Elev (ft) Elev (ft) Product <br /> MW-1 12/26/95 17 00 870 4940 40 70 None <br /> MW-1 3128196 16 87 823 ----- 41 17 None <br /> MW-1 6127196 16 88 8 84 ----- 40 56 None <br /> MW-1 9/23/96 16 85 921 ----- 40 19 None <br /> MW-1 1 211 919 6 16 88 856 ----- 40 84 None <br /> MW-1 3110/97 16 88 823 ----- 41 17 None <br /> MW-1 6130197 16 77 894 ----- 40 46 None <br /> MW-1 8/20/97 16 77 906 ----- 40 34 None <br /> MW-1 12/10/97 1 6 77 8 64 ----- 40 76 None <br /> MW-1 3/31 /98 16 79 800 ----- 41 40 None <br /> MVV-2 12/26195 18 74 955 5052 41 51 None <br /> MW-2 3128196 18 63 9 01 ----- 41 51 None <br /> MW-2 6/27/96 18 65 9 58 ----- 40 94 None <br /> MW-2 9123196 18 60 1010 ----- 40 42 None <br /> MW-2 12/19/96 18 65 9 36 ----- 41 16 None <br /> MW-2 3110/97 18 65 907 ----- 41 45 None <br /> MW-2 6/30/97 18 45 980 ----- 40 72 None <br /> MW-2 8120197 18 45 1004 ----- 40 48 None <br /> MW-2 12/10197 18 45 945 ----- 41 07 None <br /> •} MW-2 3/31 /98 18 58 877 ----- 41 75 None <br /> MW-3 12/26/95 16 67 905 49 78 40 73 None <br /> MW-3 3/28/96 16 63 8 61 ----- 41 17 None <br /> MW-3 6/27/96 16 63 922 ----- 40 56 None <br /> MW-3 9123/96 16 50 960 ----- 40 18 None <br /> MW-3 1 2/1 9196 16 58 8 93 ----- 40 85 None <br /> MW-3 3/10197 16 58 864 ----- 41 14 None <br /> MW-3 6130197 16 58 9 31 ----- 40 47 None <br /> MW-3 8120/97 16 58 948 ----- 40 30 None <br /> MW-3 12/10/97 16 58 905 ----- 40 73 None <br /> MW-3 3/31 /98 1644 839 ----- 41 39 None <br /> MW-4 8120197 18 47 973 4760 37 87 None <br /> MW-4 12/10/97 18 47 926 ----- 38 34 None <br /> MW-4 3/31 /98 18 18 8 61 ----- 38 99 None <br /> Groundwater Gradient <br /> Groundwater elevations were plotted to a known datum to prepare a groundwater contour map <br /> The groundwater flow direction was toward the north-northwest at sampling time, and a flow <br /> gradient of 0 034 was calculated Water levels have risen roughly 0 6 feet, and this rise is <br /> attributed to winter rainfall Historic groundwater flow trends typically vary from north- <br /> northeasterly to north-northwesterly <br /> Page 2 <br />