Laserfiche WebLink
<br />dlschargeswereexperlencedalongportlonsofthemalnstetnOfthe <br />South Platte River for most of the month of May and on into June. <br />Hlghwater mark data f~ thIs flood In Logan and Sedgwick COunties <br />Is contained In table 4. The Flooded Areas, Plates .3 through 28, <br />show the area flooded by this flood. <br /> <br />Table 4 <br />High Water Mark Data from the <br />South Piette RIver Flood of 1973 In <br />Logan and Sedgwick Counties, Colorado <br /> <br />PlateNa. <br /> <br />High Water <br />Mark No. <br /> <br />ElevatIon <br /> <br />Fut-ureFloods <br />Floods of the same or lerger magnitude as those that have occurred <br />could occur In the future. To determine the flood hazard posed by <br />the South Platte River In Logan and Sedgwick COunties, the IO-year, <br />50-year,IOO-year,and500-yearfloodswereanalyzed. Therroagnltudes <br />of these future floods are presented In thIs report In table 5 and In <br />the form of water surface profiles, stege-discharge curves, flood <br />width delineations, end the relationship of these future flOOds to <br />the flood of May-June 1973. <br /> <br />, <br />I <br /> <br />28 <br />" <br />" <br />" <br />25 <br />" <br />" <br />25 <br />" <br />" <br />22 <br />22 <br />" <br />20 <br />20 <br />11 <br />11 <br />11 <br />" <br />" <br />" <br />" <br />" <br />l3 <br />" <br />9 <br />8 <br />8 <br />8 <br />, <br />, <br />'" <br />8 <br />,,, <br />5 <br />, <br />. <br />. <br />. <br />3 <br />3 <br /> <br />, <br />2 <br />3 <br />. <br />, <br />6 <br />, <br />8 <br />9 <br />10 <br />" <br />12 <br />l3 <br />" <br />" <br />" <br />11 <br />18 <br />19 <br />20 <br />2l <br />22 <br />23 <br />" <br />" <br />26 <br />27 <br />28 <br />28 <br />30 <br />" <br />32 <br />33 <br />" <br />33 <br />36 <br />37 <br />'" <br />39 <br />" <br />" <br /> <br />3435.3 <br />3456.9 <br />3457.2 <br />3464.6 <br />3510.0 <br />3521.2 <br />3521.3 <br />3521.4 <br />3533.1 <br />3550.5 <br />3564.9 <br />3594.8 <br />3611.2 <br />3657.0 <br />3675.6 <br />3690,7 <br />3710.0 <br />3719.2 <br />3741.2 <br />3755.3 <br />3774.4 <br />3793.6 <br />31115.1 <br />3649.6 <br />3865.0 <br />3910.4 <br />3928.8 <br />3930.6 <br />3942.3 <br />3946.8 <br />3957.4 <br />3969,0 <br />3962.7 <br />3990.2 <br />4001.1 <br />4007.0 <br />4016.5 <br />4034.6 <br />4938.9 <br />4052.6 <br />4053.6 <br /> <br />Frequency <br />The 500-year flood Is not the largest flood that can occur but <br />the probability of larger floods Is remote. As can be see... from <br />the g8gl"'9 records for the South Platte River, discharges smaller <br />tha~ either the loo-yoer or '.l00-year floods are much more common. <br />Large floods, however, can happen; thIs was clearly demonstrated <br />by the Denver area floods of 1965, the BlaCk HIlls, South Dakota <br />areaflQOdsofJune 1972,andtheJuly 1976 floods In the Big <br />Thomp~ CanVO'" near Loveland, Colorado. <br /> <br />Hazards of LarQe Floods <br />The extent of damaQe caused bv any flood deoends on the tooogra~hy <br />of the area flooded, depth and duration of flooding, velocity of flow, <br />rate of rise, developments on the flood plain, amount of debris in <br />thefloodwater,and lcecondltlons, if Ice Isaprobletn In that <br />p~rtlcular area. A 100-year flood or a 500-year flood on the South <br /> <br />" <br /> <br />12 <br />