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<br />serving the Southwest United States 0 The Glen Canyon facilities are used <br />for peaking purposes in the system, resulting in hour by hour, weekend and <br />seasonal variations in the otherwise uniform annual release. Lake Powell is <br />still in the process of initial filling and there are interim operating procedures <br />for coordination with power production at Hoover Power Plant; coordinated <br />operations also consider water surface fluctuations at Lake Mead in connec- <br />tion with the spawning habits of the bass fishery 0 Within these overriding <br />requirements, it has not been pOSSible to give special consideration to river <br />travelers who, nevertheles s, receive many incidental benefits 0 As a service, <br />the Bureau of Reclamation furnishes prospective hourly flow charts to assist <br />experienced river guides in scheduling progress through the canyon, taking <br />advantage of the daily peak releases or the low flows as the situation war- <br />rants 0 <br /> <br />'I <br /> <br />c, <br /> <br />" <br /> <br />Figure 1 indicates the hourly amounts of discharge anticipated at <br />four of the major rapids in Grand Canyon 0 Similar charts for other rapids <br />are also available 0 <br /> <br />',' <br /> <br />\ <br />:~ <br />~:.: <br /> <br />Figure 2, a Flow-Time Relation Chart involving two typical discharges <br />through Grand Canyon, illustrates how the daily fluctuations are gradually <br />absorbed as the flow proceeds downstream. <br /> <br />',' <br /> <br />Figure 3 illustrates how river regulation at Glen Canyon Dam is <br />extending the river boating season through supplementing low period flows. <br />The shaded areas indicate a band between daily peak flows and daily mini- <br />mum flows anticipated at Lees Ferry in the year 1971. For reference purposes, <br />typical years of high (1957), moderate (1948), and low (1954) runoff have <br />been superimposed on respective illustrations (a), (b), and (c) 0 <br /> <br />" <br /> <br />,', <br />r:. <br /> <br />Under the new river regimen, the profile of the main channel remains <br />in its staircase form with relatively calm waters above and below extensive <br />rapids formed by boulders and debris deposits at the confluence of the side <br />channels. The main river still jostles and rearranges these deposits, but, <br />being limited to about 20,000 cubic feet per second, is not as powerful in <br />this respect as formerly when the discharge at times rose to over 100,000 <br />c of. so <br /> <br />. <br />t; <br />~;-. <br />", <br />" <br />~,' <br />.. '.~ <br />p" <br />'" <br />~ <br />..." <br />,,' <br /><' <br /> <br />" <br /> <br />RIVER TRAVEL <br /> <br />The availability of war surplus rubberized pontoons, strapped together <br />to form large flexible rafts capable of supporting as many as 20 passengers <br />and their gear, accounts for some of the recent popularity of river travel <br />through Grand Canyon 0 Avoiding the low flow and the extreme high flow <br />seasons, river runners formerly used wooden or fiber crafts carrying one or <br />two passengers 0 There is now only an occasional use of these small rigid <br /> <br />3 <br />