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<br /> <br />I <br /> <br />':;', <br /> <br />I <br /> <br />I <br /> <br />B~ Flood Eievation <br /> <br />I <br /> <br />Water surface elevations for ttle 10-, 25-, 5(1-, arid lOO-year fioods, <br />as d e t e t... m I n e d ate ;::L c!! C ~.. (! 5 S ~. e c t i (, n, ff! 2.. Y be f (I U n d I j, Tab i e 4 11 i::'- ! i) (1 d <br />;:'~'t.(\q\.Jency""E i 2va.t i on and D j sc Ildio-:...:jE' Da.ta I, The f I 00.] !=,j"-of j IE' da.ta <br />(sheets 1-13) shclw ~ graphical t-e ationship of water- surface <br />eleYat~ons ar(,ns .the stream r-eacrles felF the siven ft-equencies. <br />Selected typical crClss sections {r-OM different t"eaches within the <br />study area are shclwn (rn sheets 1 tht..u 6. <br /> <br />I <br /> <br />I <br /> <br />The f I Or)lj pt-of i I f2l.::. rrla')"' b(.::' u5;.ed i r: al'-ea~. l..;het-e contth('ver"sy at- i ses (lVet- <br />th(<:~ 1 00.... y f:' at" f!ol:<d t.!)undat~',/ <,;;.he'....'rl on the FiooC! F'!ain Maps. Since the <br />flood profi ie exhibits give the water surface e[eva~~on at a specifiC <br />poirlt (In t~!e refererlce I :nef t~e flood elevations can be surveyed on <br />the :J~Hollnd t.o a] 1 t~V i 2.te any rj j sc!'~erla.nc; i2S on the ba.~.e ma.p. <br /> <br />I <br /> <br />C. Flo(lded Areas <br /> <br />I <br /> <br />Flood plajn maps f s~leets 1 and ~, shaw the bOufrtiary of the IOO-year <br />fiood plain. The f:ood piain boundary was plotted using fiood contour <br />(, I E: v {il. t i (I n ~, and ~> t a. tic n i n~, f t" I) m t~! e p i 1) t i:: e d f i (1 (I d P 1'~ (! f ; I e s. . T h ! s I-fJ d. -:;:. <br />done at elevation irltervais compatible with the map corltour intervais. <br />Flood COf'ltCLI.1FS at-p. st'(IWn as w 8Sly l ines a~ 5-ft ir:tervals <br />perpendicular to tt'iP. direction of flow. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />