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<br />. <br /> <br />Slowly returns to the natural ch~nnel and constitutes the pres- <br /> <br />ent August flew which, originally wes nil. <br />This chcnge in chr rl'.cter of st.ream flow, hf's not been '?,ccom-, <br /> <br />~)lished entirely, through the ['r.ency of irrig!?tion; but is due <br /> <br /> <br />p8rtly to storage on the upper bESis <l1'e[':s. Uomplete equaliza;' <br /> <br /> <br />tion of flow is not claimed; but it has been accomplished in <br /> <br />such degree that gre~t benefit has been derived, und complete <br /> <br />equaliza~ion mude much easier. <br /> <br />Another interesting and important fact is thLt, ~fter diver- <br /> <br /> <br />sion from the streum of sufficient water to irrigate the l~rger <br /> <br />area of land now under cuI tivation in the Greet Sult Lake Basin, <br /> <br />the lake still reoeives approximately 5,000,000 acre feet of <br />~ water annuElly. ~he lake surface is now higher th~n when the <br />first water was diverted and the strea~s were free from obstruc- <br /> <br />tions and discharged di_rectly into the lrJee. An,l this in spite <br /> <br /> <br />of :0.11 the efforts tendin[': to destroy the lEl~e. <br /> <br /> <br />I would like to call specie.l attention to the foot thr:t. <br /> <br /> <br />after this long period of USe, 0"1' surplus Wl'.ter is down in the <br /> <br /> <br />lake, and not up on the water shed. lie have lots of surplus ct <br /> <br /> <br />the wrong end of the system notwithstanding Lll the efforts thet <br /> <br />have been Tl'E,de to retc.in it on the up,er land. <br /> <br />, <br />\ve thinl~ these facts are si[mificant in this case as show- <br /> <br />ing: <br /> <br />(1) That irrig~tion on the u~per areas of the stream basin, <br /> <br /> <br />is a potent and economical means of eqUE_lizing the stream flow; <br /> <br />. <br /> <br />S.L. <br />