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v m <br /> I _ <br /> (NORTH) ' <br /> (SOUTH) 1 <br /> BUILDING <br /> MW-1 4i <br /> F-11VW-1 <br /> p' �c <br /> 0' UST y 'b ' <br />' AREA ' <br /> 10' ! x o <br /> 20 44 a <br /> 20' _ <br /> 30' <br />' w30'- <br /> 40' <br /> 40' q <br /> l � <br /> -50' W U1 Q% <br /> Q% <br /> 50' / 1-.4C O w <br /> as / <br /> H 60' w <br /> 600- <br /> 4 / ` <br /> - / 70 W U]Z <br />' U 70 <br /> \ _ <br /> � � ZO �x <br /> r <br /> Lao' b U� t0 <br /> 1 8011 C) <br /> E- <br /> 1 � <br /> LEGEND <br /> SAND Z STATIC GROUND WATER LEVEL SEPTEMBER 2004 <br /> (ALSO HISTORICAL LOW GROUND WATER LEVEL) <br /> FINE GRAIN MAX Q HISTORICAL HIGH GROUND WATER LEVEL <br /> 0 005 INFERRED DOMINANT GROUND WATER FLOW DIRECTION & GrIENT (northwest) <br /> HYDROCARBON IMPACTED GROUND WATER iii <br /> MAXIMUM EXTENT OF SOIL CONTAMINATION <br /> HYDROCARBON IMPACTED SOIL MAXIMUM EXTENT OF GROUND WATER CONTAMINATION ! <br /> ® , s <br /> 20 a <br /> o xa 40 <br /> NOTE Ground water hydrocarbon inpact is inferred, as the <br /> historically impacted wells are now dry or seasonaly dry <br /> 1 <br />