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<br /> <br />offloodllJaters. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />~AIN fLOOD SEASO~ for the St. Charles River watershed is during <br />the summer months from May through August. The severest storms <br />often occur in the transitional late spring and early fall Peri_ <br />ods, floods on the St. Charles River are characteristically of <br />moderately short duration with attendant high peak flows. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />VELOCITIES Of WATER during the Standard Project flood would range <br />up toamax1:numof about 21 feet per second (approximetelyl8 <br />miles per hour) in the river's main channel, Velocities outside <br />of the main channel would vary widely, depending upon location, <br />but would reach about 12 feet per second (approximately 8 miles <br />perhovr) insorne overbank areas. Thesehighvelocitiesdvring <br />a major flood would be extremely dangerous to life and property. <br />Volocities greatar than 3 feet per second combined with depths <br />of 3 feet or more are goner ally coneidered hazardovs. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />DURATIO~ OF flOOOS on the St. Charles River is relatively short <br />as compared to those on the Arkenses River at Pueblo. In the <br />stream's lower reach, the Intermediate Regional Flood and Stand- <br />ard Project flood wovld remain above bankfull stage for about <br />23 and 29 hours, respectively. The maximum ~etes of rise for <br />these floods, 3.6 and 4.2 feet per hovr, wovld be greatest in the <br />middle reach dvo to the 10caliLedeffect of the Creenhorn River <br />whore it flows into the St. Charles River. As the flood crests <br />svbside in traveling downstream, the rates of risa would deoline <br />to 1.4 and 2.1 feet per hour, respectively, near the river's <br />mouth. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />flOOD DAMAGE PREVENTION MEASURES by local interests consist of <br />channel improvemonts and levee constrvction work, principally on <br />the Arkansas River mein stem and fountain C~eek. In so~e <br /> <br />; <br /> <br /> <br />inatances, these works have ,,'tended into the lower reaches of Wild <br />Horse_Dry Creek and Dry Creak near their mouths on the Arkansas <br />River. Regvlatory city end county zoning ordinances exist which <br />govern development in specified special flood plein districts along <br />fountain Creak, Dry Creek, Wild Horse-Dry Creck, and the Arkansas <br />River. AdditionaiflooocontrollllCasuresaraproposoointheCorps <br />of Engineers' "Report on Review SU,f"vey for flood Control and Al- <br />lied Pvrposes Arkansas River end Tribvtaries above John Martin <br />Oa.., Colorado." <br /> <br />- <br /> <br />. <br /> <br />. <br /> <br />fUTURE fLOODS of great magnitvde can be expected, but the StanM <br />dard Project flood repreoents the reasonable vpper limit of ex- <br />pected flooding. floods the size of the Intermediate Regional <br />flood have occurred in the pest ~nd will recvr in the future. <br />Comparisons between fvture ond past floods havo not been made be- <br />Cause interim flood plain development and changing Channel condi- <br />tions generally depreciate the practical value of such date. Con_ <br />sidering that comprehensive plans for the city and county of Pueblo <br />envision e future of vigorovs growth, it can be reesonably conw <br />eluded that futvre flood damages ~ould be more extensive dve to tho <br />continuing development and greater us~ of land in the flood plains. <br /> <br />, <br /> <br />. <br /> <br />. <br /> <br />, <br />