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<br />ho~ever, attenuates rapidly on the South Platte River downstream <br />from the contributing trIbutaries due to valley storage of the <br />floodwater, <br />Thegenerlll ralnstormfloodsresultfromralnfalloverllreas <br />at large areal extent. Rainfall from this type of storm may occur <br />over several days, Because of this time duration, the affected <br />streams rise relatively slow; sometimes over a period of several <br />days. The duration of the flood period also Is sometImes of con- <br />siderable length. Because of the large areal extent of rainfall, <br />more tributaries contribute to the peak discharge on the South <br />Platte River. This results In IncreasIng discharge progressively <br />downstream over a consIderable length of the South Platte River. <br />However, downstream from the contrIbutIng tributaries, the effects <br />of valley storage cause flood discharge attenuation. <br />Erosive effects can be considerable in the event of any flood <br />regardless of Its origin. Floods resulting from Intense rainstorms <br />typically create severe erosion damages in 1l Short periOd of time <br />due to tho relatively large peak dIscharge and high velocity of <br />the floodwater. ErOSion damages from snowmelt or general rainstorm <br />floods usually result from prolonged exposure of the floodwater <br />because of the long duration typical of these floods. <br />Intense rainstorm floods as well as general raInstorm floods <br />have occurred on the South Platte River. Examples of the Intense <br />storms are the 1965 events on Plum Creek and BljouCreekand the <br />1976 ~ent on the Rig Thomrson River. Ex~rnples of the I~rg"r more <br />gonorallzed storms aro the 1969 ~nd 1973 events producing flooding <br />on the South Platte River. <br /> <br />Past Flood~ <br />Several floodS have occurred along the South Platte River in <br />Morgan and Washington Counties. Tables 2 through 4 IndIcate ye~rly <br />p9~k discharges experienCed ~t the three stre~m gaging stations oper- <br />~ted in th" past by th" \), S. Goological Survey In Morgan County. <br /> <br />, <br /> <br />South <br /> <br />Table 2 <br />Annual Peak Discharge for the l/2/ <br />Platte River near Woldona, Colorado- <br /> <br /> "", Olschar!1e <br /> <C.f.s.) <br />" ,,' 1957 14,200 <br />" .., 1958 8,840 <br />6 JyO 1961 7,740 <br />19 JyO 1955 18,800 <br />" JyO 1969 17,000 <br />14 JyO 1970 14,000 <br />" 'pc 1971 7,400 <br />e 'OV 1973 26,800 <br /> <br />11 <br /> <br />From U.S.G.S. Gaging Station located 400 feet downstream from <br />Colorado State Highway 144 ~nd 2.8 miles southeast of Weldona. <br /> <br />y <br /> <br />Only those years having a peak discharge of 5,000 c.l.s, or <br />greater are indicated. <br /> <br />For period of gaging record, see table I. <br /> <br />6 <br />