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<br />r--- <br />~ <br />00 <br />-C' <br /> <br /><.: <br /> <br />I:R <br /> <br />""" <br /> <br />-' <br /> <br />. <br />11 <br />:1 <br /> <br />\ Ii <br />., <br /> <br />.. <br />.. ! <br /> <br />.. <br />I; I <br /> <br />:) <br /> <br />," <br /> <br />: I <br /> <br />!; <br />, <br />j:~ ,j <br /> <br />I: <br /> , <br /> .[ <br /> ': <br />; , <br /> " <br /> , <br /> " <br /> <br />I' <br /> , <br /> I <br /> " <br />'I. <br /> <br />, <br /> <br />. <br /> <br />. <br /> <br />36 <br /> <br />a half (3 1/2) before. <br /> <br />;i <br /> <br />" <br /> <br />!lR. Gl\RNER: Now, do you want to go above? <br /> <br />Ii <br />,I <br /> <br />MR. BRANTINGHAN: If we can see it I want to <br /> <br />,i hear about it. <br /> <br />MR. GARNER: Below Antique Rock, by our <br /> <br />reading curve, our normal high water mark is about three <br /> <br />. <br /> <br />!: <br /> <br />fifty anu a half (350 1/2). And the flow gets attenuated <br /> <br />somewhat in its channel from Parker down there. But it's <br /> <br />still in the neighborhood of eighteen (18,000), seventeen <br /> <br />(17,000), eighteen (18,000), nineteen thousand (19,000) and <br /> <br />we can't tell you within inches. <br /> <br />HR. BRANTINGHAM: Are we looking at basically <br /> <br />the same amount above and below there, just by parameters? <br /> <br />MR. GARNER: Basically the same amount of <br /> <br />water. <br /> <br />HR. BRANTltiGHAl<l: As far as the level of the <br /> <br />River will go up and down at anyone time -- <br /> <br />MR. GAffilER: The level of the River would not <br /> <br />fluctuate. <br /> <br />MR. BRANTINGHAH: -- it doesn't change when <br /> <br />we get above Headgate Dam? <br /> <br />MR. GARNER: Oh, .when you get above the gate, <br /> <br />., . <br />.,' ,: you I ve got -- <br /> <br />~,' <br /> <br />MR. BRANTINGHA/1: You've held the meetings -- <br /> <br />let's see, I've been to twO (2) other meetings, and in the <br /> <br />" I <br />