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<br />A number of irrigation ditches; such as the Treasure Pass, Rober-Lohr <br />and Fachs ditches convey water across natural drainage boundaries from <br />the Colorado River Basin. A number of reservoirs also regulate flow <br />in the basin. The Rio Grande is affected by the Beaver Creek, Santa <br />Maria, Rio Grande and Continental reservoirs. <br /> <br />2.3 Principal Flood Problems <br /> <br />While slopes are steeper in the upper drainage basins, the dense <br />vegetation in these areas serves to reduce rainfall runoff. A greater <br />percentage of runoff is permitted by the spa rse vegeta ti on of the <br />foothills and pasture land at the lower elevations. Consequently, the <br />majority of the flood problems in the study area are caused by rapid <br />snowmelt. This type of flooding has a long duration runoff which <br />results in a continuous rise in water level thus producing a high <br />runoff vol ume. <br /> <br />Flood potential al so exists from long and short duration rain storms. <br />These types of floods are characteri zed by hi gh peaks, small vol umes <br />and short duration. The potential for the most severe flooding is <br />created by the combination of rapid snowmelt with long duration rain- <br />fall . <br /> <br />Information on past flooding is based on newspaper accounts and inter- <br />views with longtime residents of the area. Large floods occurred at <br />Monte Vi sta in 1884, 1905, 1911, 1927, 1949, 1957 and 1970. These <br />floods have caused major damage, disrupting highway and railroad <br />traffic and communication services, drowned livestock, destroyed <br />agricultural lands, roads, bridges and buildings. <br /> <br />The fl ood of 1884 is consi dered the most severe fl ood known in Monte <br />Vista, with an estimated peak discharge of 20,000 cubic feet per <br />second (cfs) at Al amosa, Colorado. The Colorado State Engineers <br />Annual Report of 1911, proposed melting snow and rainfall as the cause <br />of the flood in 1911. This flood has an estimated peak discharge of <br />14,000 cfs. <br /> <br />In June of 1927, a peak flow of 18,500 cfs was recorded in Monte <br />Vista. Flooding was due to four days of cloudbursts and incessant <br />rains. Floods in the Monte Vista Area generally ranged from 4,000 to <br />7,000 cfs between 1926 and 1967. <br /> <br />2.4 Flood Protection Measures <br /> <br />The City of Monte Vista has no existing regulations or ordinances <br />concerning floodplain management or protection measures other than <br />those of the Uniform Building Code, 1976 edition. <br /> <br />3.0 ENGINEERING METHODS <br /> <br />For fl oodi ng sources studi ed in deta il in the community, standard hydro- <br />logic and hydraul ic study methods were used to determine the flood hazard <br />data required for this study. " Flood events of the magnitude which are <br /> <br />5 <br />