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<br />The graphs on pages 27 and 28 illustrate some of the pertinent historical facts <br />related to the amounts of water produced by the Colorado River System above Lee <br />Ferry, Arizona, the compact division point between the Upper and Lower Colorado <br />River Basins. The first graph, on page 27, is entitled Colorado River Flow at Lee <br />Ferry, Arizona. The top of each vertical bar represents the estimated virgin flow of <br />the river, Le., the flow of the river in millions of acre-feet past Lee Ferry for a given <br />year had it not been depleted by activities of man. Each vertical bar has two <br />components: The lower shaded part represents the estimated or measured historic <br />flow at Lee Ferry, and the difference between the two sections of the bar in any <br />given year represents the stream depletion, or the amount of water estimated to <br />have been removed by man from the virgin supply upstream from Lee Ferry. It is <br />worth noting that in 1977, and again in 1981, the historic flow at Lee Ferry <br />exceeded the virgin flow. Beginning in 1962, part of this depletion at Lee Ferry was <br />caused by the retention and storage of water in storage units of the Colorado River <br />Storage Project. The horizontal line (at approximately 14.8 million acre-feet) shows <br />the long-term average virgin flow from 1896 through 2004. Because the Colorado <br />River Compact is administered on the basis of running averages covering periods <br />of ten years, the progressive ten-year average historic and virgin flows are <br />displayed on this graph. <br /> <br />The second graph on page 28, entitled Lee Ferry Average Annual Flow for <br />Selected Periods, is a graphical representation of historic and virgin flow averages <br />for several periods of record. The periods of water years selected were those to <br />which reference is usually made for various purposes in documents pertaining to <br />the Colorado River System. <br /> <br />Several important hydrologic facts are apparent from these two graphs on pages <br />27 and 28. <br /> <br />(1) A vast majority of the high flows occurred prior to 1929. <br /> <br />(2) Since the 1924-1933 decade, the progressive ten-year average virgin flow <br />has not exceeded the average virgin flow except in the 1941-1950 and the <br />exceptionally wet 1975-1984 through 1984-1993 decades. <br /> <br />(3) For the period 1896-1921, which is prior to the Colorado River Compact of <br />1922, the average virgin flow was estimated to be 16.8 million acre-feet <br />per year, which is considerably greater than for any other period selected, <br />including the long-term average. A stream-gaging station at Lees Ferry, <br />Arizona was not installed until 1921. Thus, the virgin flow at Lees Ferry <br />prior to the 1922 Compact is estimated based upon records obtained at <br />other stations, e.g. the stream gage on the Colorado River at Yuma, <br />Arizona for the period 1902-1921. <br /> <br />(4) For the longest period shown, 1896-2004, the estimated average annual <br />virgin flow is 14.8 million acre-feet and the average annual historic flow is <br />12.0 million acre-feet. <br /> <br />(5) For the next longest period, 1906-2004, the estimated average annual <br />virgin flow is 14.8 million acre-feet and the average annual historic flow is <br />11.9 million acre-feet. Many of the early records for this series of years, <br />as well as for the 1896-2004 period, are based upon the estimates of <br />flows made at other gaging stations, as mentioned in (3) above. This <br />average is about equal to the 15.0 million acre-feet estimated for the <br />1906-1967 period which was used as the basis for justification of a water <br />supply for the Central Arizona Project authorized in 1968. <br /> <br />(6) The estimated average annual virgin flow during the 1914-2004 period is <br /> <br />25 <br />