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Figure 11 is a hydrograph of ground water elevations in the <br />study area compared with stage elevation of the Green River. <br />Clearly, all wells shown have water elevations lower than the <br />Green River, and all have similar rates and magnitudes of <br />drawdown. We believe that these wells are connected to the Green <br />River and receive some water from it. In late summer ground <br />water levels in the study area rise due apparently to continued <br />discharge from springs and reduced evapotranspiration. <br />z <br />0 <br />~_- <br />Q <br />W <br />W <br />4834 <br />4832 <br />4830 <br />4828 <br />4826 <br />o E9 <br />v ^ E10 <br />o E11 <br />v-v Green River <br />x E7 <br />+ E6 <br />• E5 <br />x + <br />x <br />o } <br />^ °~-v <br />a x <br />x ~ v <br />0 <br />x <br />g x <br />o + <br />0 <br /> 0 <br />• ~ ~ <br /> o <br /> ® g <br /> • <br /> <br />^ <br /> <br />JUNE JULY AUG SEPT <br />Figure 11. Hydrographs of the Green River and ground water at <br />our stations during 1993. <br />18 <br />