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<br />INVESTIGATIONS AND ANALYSIS <br />Interpretation and Use of Report <br />A. Frequency and Discharge <br />The 10-, 50-, 100-, and 500-ye~r fl ood events are used as the t1 oOd <br />frequencies for this flOOd plain analysis, Thus, the data developed in <br />this report wi 11 be suitable not only for reg~latjon purposes, and H.B. <br />1041 destgnationbutalsoforFederal lnsuranceAdministrationflood <br />ins~rance studies co~d~cted by the Federal Emergency Management Agency. <br />These ~arious flood events ha~e an average occurrence of once in the <br />numb~r of years as indicated. For e~ample, the 100_y~ar flOOd occurs, on <br />the average, once in a lOa-year period, and has a one percent chance of <br />being equaled or exceeded in any given year. <br />The particular uses for the various flood events in addition to tho se <br />stated above are as fOllows: <br />lO_Year and 50.Year Flood Events <br />lnformation regdrding these lower frequency floods is especially <br />useful for future engineering studies and land use planning purposes <br />related to minor road systems, minor channel improvements, the location of <br />par~s and recreational facil it ies, agricultural lands, and appurtenant <br />structures. The use of the lower frequencey floods may be considered in <br />pl anni ng fl Ood prev~nt i on projects to protect agri cul tura 1 dr,,~~, or other <br />property w~ere risk to life is not a factor. <br />laO-Year Flood Event <br />The IOO-year flood event may be used in lieu of lower frequencies for <br />engi neering design purposes where greater s~curi ty from structure fai lure <br />is desired. <br /> <br />However, the most important use of the lOa-year flOOd event lies i~ <br />flood plalnmanagelTlent and land use planning as set forth in the sta te <br />statutes, The State of ColoradO considers the 100-year frequency flOOd as <br />the flOOd event to be used in desig1ing and protecting structures and <br />dwellings for human occupation. Therefore, all flood plain regulations <br />are based upon the lOO.year flood, <br />500-Year Flood Event <br />The 500-year flood event is useful in making the public aware that <br />floods larger than the laO-year flOOd can and do occur. Just because a <br />person is l1ving above the laO-year flood boundary does not mean that he <br />is completely safe from flooding. The 500-year flood event can also be <br />used for regulating high risk developments within the flood plain such as <br />nuclear power plants, or the storage or manufacture of toxic or explosive <br />mdterials. <br />B. FlOOd Elevation <br />Floodcreste1evdtions fortne10-, 50-, 100-, anct 500-year floOdS, <br />as determined at edch cross section, may be found in Table 1 "Flood <br />Frequency-Elevation and DischugeData", Flyures, 1 through 5, show a <br />graphical representation of high water elevations at typical valley cross <br />sections. Water surface elevations computed at each cross section were <br />used to prepare flood profiles, sheets 1 through 23, which ShOw the <br />streambed elevation in relation to ~ater surface elevations for the 10-, <br />50-, 100-, and 500-year frequency floods. <br />The flOOd profiles may be used in areas where controversy arises over <br />the laO-year flood boundary s~own on the FlOOd Plain Maps. Since the <br />flood profile e~hihits give the water surface elevation at ~ specific <br /> <br />-11- <br /> <br />-12- <br />