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<br />4 <br />4 <br />4 <br />4 <br />4 <br />4 <br />4 <br />4 <br />~ <br />~ <br />~ <br />~ <br />. <br />. <br />. <br />. <br />Well Head . <br />7500 . <br />250 . <br />000 . <br />750 . <br />500 . <br />250 <br />'000 · <br />~750 . <br />500 . <br />250 . <br />000 . <br />750 . <br />500 . <br />250 . <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />Figure 3.9(b) <br />\Vater LeH'ls in the Lower [)al-HOn Aquifer in 2{)oO~Simulated <br /> <br />rr= <br /> <br />- <br /> <br /> <br />. <br /> ~ <br />" ~1,.." ,< <br /> , <br /> <br />Legend <br /> <br /> <br />~ <br /> <br />, . <br /> <br /> <br />· Dry Cell <br /> <br />I <br /> <br />t1n.r:l,~ ?'~ <br />'!l ,;rv''''L <br />.\.. \ <br />-',. .' ~ <br />.r' .' <br />r--- <br /> <br /> <br />~:~ -~:~~~ <br />,~# <br /> <br />1 <br /> <br />Water levels in the Lower Dawson aquifer in 2000 (al Observed with the dots indicating <br />loc'ations of wells used 10 generate the contour maps and (b) Simulated. Also identitied <br />in (b) arc the well locations for the hydrographs presented in Figure 3.8. <br /> <br />Page 3.25 <br /> <br />