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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />Fj~ure 3.9(0) <br />Water Leyels in the Lower ()awson Aquifer in 2000-0bsen:ed <br /> <br /> <br />- <br /> <br /> <br />.; <br /> <br />\ <br /> <br />- <br /> <br />~J!P <br />.... ~ <br />--~ <br /> <br />,. <br />,. <br />" <br />,. <br />~ <br />~ <br />~ <br /> <br />. <br /> <br /> <br />. <br /> <br /> <br />-- <br /> <br />- <br /> <br />.... <br /> <br />~ <br />...... -',500" <br /> <br /> <br /> <br /> <br />Water levels in the Lower Dawson aquifer in 2000 (al Observed with the dots indicating <br />locations of wells used to generate tht' contour maps and (b) Simulated. Also identified <br />in (b) arc the well locations for the hydrographs presented in Figure 3.8. <br /> <br />Page 3-~~ <br />