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10, and 5. The hydrographs of stations 1, 6 and 10 are quite <br />similar even though our wells are augured into the underlying <br />gravels which we presumed were directly connected to the Gunnison <br />River. <br />Figure 9 includes hydrographs for the southern side of the <br />study area. Station 7 again, is the Gunnison River. Station 20 <br />is a small man-made pond and retains very stable water levels <br />that are higher in elevation than the River. This hydrograph is <br />very similar to that of station 10 on the north side of the River <br />and indicates that many features on the main portion of the <br />floodplain can maintain water levels far above that of the river. <br />-~--~ <br />4522 <br />4520 <br />~_o <br />0 <br />v <br />v <br />Gunnison River <br />v <br />0 <br />^-^ C E 19 <br />a-o CE20 <br />~-~ CE23 <br />v-v CE7-River <br />z <br />O <br />Q <br />W <br />_._J <br />W <br />4518 <br />4516 <br />v <br />_~~ <br />:~ <br />\~~~ <br />JUN JUL AUG SEP OCT <br />Figure 9. Hydrographs for stations in the southern study area. <br />15 <br />