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FLOOD05184
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Last modified
1/25/2010 6:48:32 PM
Creation date
10/5/2006 1:18:55 AM
Metadata
Fields
Template:
Floodplain Documents
County
Boulder
Community
Boulder County
Stream Name
Lower Boulder Creek
Basin
South Platte
Title
Flood Hazard Area Delineation
Date
3/1/1983
Prepared For
Boulder County
Prepared By
UDFCD
Contract/PO #
&&
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />- FUTURE FLOODS - <br /> <br />The following paragraphs contain a general description of flooding conditions <br />along Lower Boulder Creek: <br /> <br />Flood Frequency and Discharge <br /> <br />The 100-year flood is based upon recorded historical precipitation and other <br />valid data and, statistically, has a one percent chance of being equalled or <br />exceeded during anyone year. The 100-year flood is also commonly referred <br />to as the base flood, regulatory flood, and intermediate regional flood. <br />Floods of this magnitude or greater have occurred on Boulder Creek in the <br />past and will occur in the future. <br /> <br />Valley View Road to North 75th Street - <br /> <br />This 3.9-mile study reach is characterized by numerous gravel pits, dikes <br />and berms resulting in a very irregular flood boundaries. Numerous island <br />areas and dikes associated with the gravel mining operations are shown on the <br />floodplain maps. Cross Section Nos. 86 to 129 represent this study reach. <br />Floodplain limits are shown on Sheets 2 through 6 and the water surface profiles <br />on Sheets 18 and 19. <br /> <br />The discharge probability profiles in Figure 3 graphically represent the <br />relative magnitude of the major flood events. This information is useful not <br />only for regulating future floodplain construction, but also for planning <br />and engineering of channel improvements and flood protection facilities. <br /> <br />The stream in this reach flows generally in a northeast direction. Stream <br />crossings include the Union Pacific Railroad, Valmont Drive, North 66th Street, <br />two access drives, and North 75th Street. The average 100-year floodplain <br />widths range from 1500 to 4000 feet. The Union Pacific Railroad generally <br />parallels the southern floodplain boundary. <br /> <br />The 100-year flood is identified by the Urban Drainage and Flood Control <br />District, the Colorado Water Conservation Board and the Federal Emergency <br />Management Agency as the flood magnitude used for the regulation of flood- <br />plains and for the design of improvement facilities. In Colorado, the <br />100-year floodplain represents an area of state interest as defined in H.B. 1041. <br /> <br />South Boulder Creek and Fourmile Canyon Creek are the major tributaries <br />within this study reach. At the South Boulder Creek confluence a special <br />analysis was performed to determine the divided floodway and flow splitting <br />assumptions for Cross Sections 119 through 128. The 100-year discharge in <br />the channel area of Boulder Creek was estimated at 4,800 cfs as compared <br />with a total discharge of 13,300 cfs downstream of the South Boulder Creek <br />confluence. The user of this report should contact Boulder County regarding <br />floodway requirements for this area. <br /> <br />Flooded Areas <br /> <br />The Appendix of this report contains the Flood Hazard Area Delineation Maps <br />showing the limits of the 100- and SOD-year floodplains (Sheets 2 to 17). <br />Water surface profiles are shown separately on Sheets 18 to 23. Table III, <br />"Floodplain Reference Data," which follows the report sununary, presents dis- <br />charge information and computed water surface elevations for the 10-, 50, <br />and SOD-year flood events. Table IV, "lOO-Year Floodplain and Floodway <br />Reference Data," whi ch foll ows Table I II, presents i nformati on perti nent to <br />the regulation of the 100-year floodplain. Specific information regarding <br />flood discharges, flood elevations, widths, and other descriptive data is <br />listed in Table IV. <br /> <br />As stated previously in this report, a conservative analysis was used for <br />the reach considering the unknown integrity of the diking systems used in <br />the gravel mining operations. The hydraulics assume that the diking system <br />is intact and the low-lying areas landward of the dikes are ineffective for <br />conveying floodwaters. <br /> <br />10 <br />
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