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<br />WATER LEVEL\ WELL 125Q5 <br />4.665 f- \ I I: t ^ /' . ,( <br />i r~\ II \. 1'\. ,fl, 1\../ \ ! \ r', r---"', <br />\~'I'l ~' Ii \1'" \1 ,{ \1 "''-..If <br />L... \ , . "" "I J \i \ I " " <br />4,660 .- : I ^ :. II i" J <br />:",' . <br />::. <br />lJi <br />1 ~, <br />4.655 ~ ~ " 11 .A I \\ / \ II <br />rJ Iw~\~ j)' ~j 'y....J \ f~ I' I It <br />4.650 ~ 1 / .I.".. \ \ / <br />DISSOLVED SOLIDS V l--.J <br /> <br />4,670 <br /> <br />-' <br />w <br />> <br />w <br />-' <br /><( <br />w <br />en <br />w <br />> <br />o <br />CD <br /><( <br />I- <br />w <br />w <br />u. <br />~ <br />ui <br />o <br />:J <br />I- <br />~ <br /><( <br />-' <br />w <br />> <br />w <br />-' <br />ri:. <br />w <br />I- <br /><( <br />:i: <br /> <br />4.645 - <br /> <br />4,640 <br /> <br />4.605 <br /> <br />4.600 - <br /> <br />4.595 ~ <br /> <br />, <br /> <br />, <br /> <br />, <br /> <br />4,590 <br /> <br />, , <br /> <br />, , <br /> <br />, <br /> <br />, <br /> <br />, , <br /> <br />, <br /> <br />1~ 1~5 1m 1~ 19n 19~ 1~1001'~ 1~3 1~ 1~ 1~ <br /> <br />, , <br /> <br />, <br /> <br />, , , , <br /> <br />, <br /> <br />WELL 208KO <br /> <br />WATER LEVEL <br />\ ~ .Ii r.\ <br />" I. I. <br />'\ ' I' ",' . <br />j' t \ f \ <br />\ .-/ \, \/ \., <br />...." ~ \J " <br /> <br />, <br />\ <br />. I~ <br />I 1\ <br />V <br /> <br />t <br />t t\ ,,"'\ <br />I) ~ I ' <br />k 1 I <br />/1' <br />4,580 - Y <br />DISSOLVED SOLIDS <br /> <br />t <br />II <br />,\ t <br />'~ ' \ I' <br />\ 'I I <br />'\11 \ f'l \ M <br />I I I I I <br />.. ., I <br />\1 . I \ <br />ll. .I.; \.. <br /> <br />4,585 - <br /> <br />4.575 <br /> <br />, <br /> <br />, <br /> <br />, , <br /> <br />, , <br /> <br />, <br /> <br />1974 1975 1976 1977 1976 1979 1980 1981 1982 1983 1984 1985 1986 <br /> <br />Figure 9. Historical water-level altitudes and concentrations of dissolved solids in water <br />from wells 125Q5 and 208KO, located in the Grand Valley (Jack Cunningham, Bureau of <br />Reclamation, written commun., 1992), <br /> <br />6,000 <br /> <br />5,000 <br /> <br />4,000 <br /> <br />3,000 <br /> <br />2,000 <br /> <br />1,000 <br /> <br />12,000 <br /> <br />10,000 <br /> <br />8,000 <br /> <br />- 6,000 <br /> <br />4,000 <br /> <br />2,000 <br /> <br />o <br /> <br />cr <br />w <br />I- <br />::J <br />cr <br />w <br />c.. <br />en <br />:::; <br /><( <br />a: <br />" <br />::J <br />-' <br />:::; <br />Z <br />Z <br />o <br />~ <br />a: <br />I- <br />Z <br />w <br />() <br />Z <br />o <br />() <br />en <br />Cl <br />::J <br />o <br />en <br />o <br />w <br />> <br />-' <br />o <br />en <br />en <br />is <br /> <br />14 Physical, Chemical, and Biological Data lor Detailed Study ollrrlgollon Drainage In the Uncompahgre Project Area and <br />In the Grand Valley, West-Central Colorado, 1991-92 <br />