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main stem on the south bank. These three rivers are sm~ll perennial streams in t~eir <br />mountainous headwater reaches, but as they progress through the foc~thills to the rolling plains, <br />the base flows aze depleted by diversions for urigation. The river channels widen with poorly <br />defined banks and low flow channels meander through the valleys. i:~e Huerfano River <br />confluence is at Boone about four miles south of Avondale. The Api.shapa River confluence is <br />just downstream of Fowler. The Purgatoire River confluence is just south of Las Animas. <br />Three smaller tributaries are the St. Charles River, Timpas Creek and. Horse Creek. The St. <br />Chazles River enters the Arkansas River from the south just downstream of Pueblo. Timpas <br />Creek enters from the south at Swink, about four miles downstream af Rocky Ford. Horse <br />Creek, enters from the north just upstream of Las Animas. The permeability of the soil and the <br />absence of well-defined watercourses in these tributary ~vatersheds te:nd to reduce the runoff. <br />5urface water discharge into the main stem is minor except in cases of extreme precipitation. <br />Timpas Creek has a drainage area of 496 square miles. Watershed elevations extend from 5,400 <br />feet at the headwaters to 4,120 feet at the stream gage near Swink. Horse Creek has a drainage <br />area of 1,403 squaze miles. The elevation of the Horse Creek watersh.ed ranges from 6,600 feet <br />to 4,200 feet. There aze no significant flood control structures on the:ce tributaries. T'he St. <br />Charles Reservoir is just south of Pueblo, but it is not actually on the St. Charles River. <br />The State of Colorado has identified flood prone azeas in 267 cities ard towns am~ng all of its 63 <br />counties. There are over 250,000 people living in floodplain azeas of the state. The value of <br />property, structures, and contents located in identified floodplains is estimated to be over $11 <br />Billion (1996 state estimate). Based on property damaoe data from 1896 to 1984, the average <br />annual flood losses in Colorado aze estimated to be $17,600,000. Cu~ulative fload losses for the <br />most damaging floods in Colorado between the turn of the century and 1993 include 331 people <br />killed and $3.3 Billion (1995 state estimate) worth of properry damage. United St,ates Presidents <br />have declared a major flood disaster within Colorado in 9 out of the last 32 yeazs between 1965 <br />and 1999 (1965, 1969, 1970, 1973, 1976, 1982, 1984, 1997, and 1999). <br />FLOOD OF APRIL 29,1999 <br />A lazge regional storm produced heavy rainfall in southeast Colorado and northeast New Me~co <br />from Thursday Apri129, 1999 through Sunday May 2, 1999. Localized flooding occurred <br />throughout the region. Numerous roads and bridges were flooded or damaged. Homes were <br />flooded in Fountain/Manitou Springs beginning on the evening of Apr;.l 29, 1999. The unusually <br />large volume of runoff produced by the storm resulted in more erosion damage along Fountain <br />Creek than any previous flood. The Arkansas River began flooding on April 30, 1~99 affecting <br />homes east of Pueblo near Avondale. The flood reached a new stage of record at Avondale on <br />May 1, 1999. Between May 1 and 2, 1999 floodwaters sp:read downstream affectirig homes in <br />Rocky Ford and La Junta. Las Animas was spazed damage to homes. Trinidad Dam on the <br />Purgatoire River and John Martin Dam on the Arkansas River both rose to new record pool <br />reservoir elevations. On May 17, 1999, the President signed DR#1276 declaring the ten counties <br />of Otero, Bent, El Paso; Larimer, Pueblo, Las Animas, Crowley, Kiowa, Elbert, and Freemont in <br />Chap~`er 1 - Introduction <br />Post Flood Assessment Report ~ 2 l~rajt Revised Q9I09/99 <br />