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Maximum flows for-May and June for the period of record are l <br />shown in Figure 11.-This figure shows the rarity of flows, <br />greater than 40,000 cfs'since 1959, and how common they were <br />prior to-that date.- Overbank flows occurred on the average once <br />every other year historically, yet are now rare events <br />precipitated only by extreme mountain snowpacks. It also. <br />illustrates-that flows such as occurred-in 1993 were a regular-. <br />.:event in the early time period. <br />Colorado River of Cisco <br />80 <br />70 <br />~ 60 <br />[n <br />Li <br />U <br />~ 50 <br />N <br />O C <br />J ~ 40 <br />l.~ ~ <br />. ~ ~ <br />~_ 3U <br />X <br />Q 20 <br />~ ~' <br />LO <br />0 <br />1, „ ~yta iy~a 19aa 1954 1964 1974 1984" 1994 <br />191,9 1929 1439 1949 1959 1969. 1.979 1989 <br />~ =-~--MAY ~ -JUNE <br />Figure 11. 'Maximum flows for"May-and June during-the period of <br />record. <br />During-high Colorado River .flows the river extends from <br />:north to"south across the entire study area connecting the. <br />wetlands with the whole river system.. However, once the river <br />water retreats, two completely independent hydrologic systems <br />occur; one feeding the Colorado River and a ground and surface <br />--water system feeding the Moab wetlands.-.Due to changes Colorado <br />" River flood frequency since 1959,-the mixing of these waters <br />rarely occurs. This is important in trying to understand how <br />fishes could interact between these two hydrologically distinct <br />21 <br />