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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 />feet (msl) at Mount Gunnison to approximately 6000 feet (msl) at the lower end of the <br />study, Vegetation and topography vary widely with elevation and landuse, The lower <br />river valley is primarily in agricultural land use with heavy vegetation in the river <br />corridor and on the channel sidebanks, The channel is deep and well defined in some <br />locations with lower banks and a smaller cross-section where it passes through fields and <br />has been manipulated to accommodate farming practices. <br /> <br />The U.S, Geological Survey published an open-file report (84-137) of stream statistics <br />that shows a stream gaging station on Minnesota Creek near Paonia with 11 years of data <br />(1936-1947), The station (number 09134000) is listed as having a basin area of 41.5 <br />square miles, mean basin elevation of 8500 feet and mean annual precipitation of 30.4- <br />inches. Land use for this basin is shown at 40-percent forest, 10-percent agricultural, 49- <br />percent range and I-percent urban use, A second gage noted as Minnesota Creek at <br />Paonia (number 09134050) had reported flows from 1976-1979, <br /> <br />5.0 tOO-YEAR FLOOD FLOW <br /> <br />The 100-year flood flow given in the USGS Report for the gaging station on Minnesota <br />Creek near Paonia is 345-cfs based on 11 years of stream data, The gage noted as <br />Minnesota Creek at Paonia show a 100-year flood flow of912-cfs based on 3-years of <br />stream data, The 1983 FEMA study used 1375-cfs for the flood flow on Minnesota <br />Creek based on regional floodflow/frequency analysis, For the purpose of this study we <br />have used the FEMA 100-year flood flow of 1375-cfs, although an analysis was <br />performed with the 912-cfs (for comparison only) and generally showed computed water <br />surface elevations of approximately I-foot lower, <br /> <br />6.0 METHOD <br /> <br />The hydraulic analysis utilized the D,S, Army Corps of Engineers HECRAS model to <br />determine water profile and flow characteristics, A field survey was used to determine <br />geometric conditions for the creek, overbanks and culverts for input to the HEC-2 model. <br />Roughness factors (Manning's "n" values) were determined based on visual observation <br />and were estimated at 0.15 for heavily vegetated overbanks and 0,035 for the channel. <br /> <br />The flow regime for this section of the creek is mixed with sections of subcritical and <br />sections of critical flow, The slope area method was used to determine starting water <br />elevation at the upstream cross-section, The model interpolated cross-sections between <br />measured cross-sections where necessary due to changes in channel conditions. Three <br />culverts were modeled where the County Road (050 Road) crosses the creek, <br /> <br />The hydraulic analysis was made based on unobstructed flow, All elevations are <br />referenced to the NGVD Datum 1929, <br /> <br />2 <br />