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<br />Corps of Engineers by the National Weather Service and is developed from major <br />storms that have occured in the region. <br /> <br />, <br /> <br />In the 1940's, local interests constructed a levee system along the Rio <br />Grande to protect Alamosa. The levee system begins just north of Alamosa and <br />continues to the south side of the community. Since the construction of these <br />levees, their structural integrity has been reduced to the point where they <br />are essentially no more than spoil banks. Trees growing on the levees have <br />further reduced their effectiveness by causing piping through the levees <br />during high flows. Residential development in the northwest part of Alamosa <br />and East Alamosa also has contributed to the increasing flood problem. Flows <br />equal to or greater than the 10-year event (4,600 cfs) will outflank the <br />existing levee system and cause damage to Alamosa and East Alamosa. <br /> <br />.... <br /> <br />B. Historical Floods: The earliest recorded flood was in 1869. Little <br />is known about this flood other than some damage did occur in Alamosa. A <br />flood in 1884 was caused by the melting of a heavy snow cover augmented by <br />heavy rains. The flood of 1884 was caused by the melting of a very heavy snow <br />cover. This flood peaked on June 14th and 15th, and was probably the flood of <br />record. The flood of 1905 was the only destructive flood in which rainfall as <br />not a factor. The flood of 1911 was the only one recorded in the upper Rio <br />Grande Basin that was caused wholly by heavy rains. The flood of 1927 was the <br />highest since stream gage records have been kept. This flood was caused by <br />melting snow and increased by precipitation. <br /> <br />More recently, high flows occured in 1979, 1985, and 1986 in the Alamosa <br />area. Only a successful flood fighting effort in all three years prevented <br />substantial damage within the study area. <br /> <br />V. EXPECTED FUTURE WITHOUT CONDITION <br /> <br />Without the implementation of flood control measures, the communities of <br />Alamosa and East Alamosa will remain suseptable to a severe flood threat from <br />high flows of the Rio Grande. Existing average annual damage in the study <br />area are currently estimated at $1,093,000. Assuming that no new residences <br />or businesses moved into the 100-year floodplain, damages and interruption of <br />services will continue in the future. Without a flood fighting effort these <br />damages will begin to occur between the five and ten year event. The existing <br />levee system, while providing minimal protection, will continue to <br />deteriorate, and provide even less protection. <br /> <br />VI. FLOODPLAIN INVENTORY <br /> <br />A. Area of Consideration: The flood plain of the Rio Grande in the <br />vicinity of Alamosa, Colorado, encompasses approximately 5,000 acres. For the <br />purpose of this analysis, the flood plain divided into two economic reaches. <br /> <br />Reach 1: Locted on the South Bank of the Rio Grande, Reach 1 is urbanized <br />and includes the downtown Alamosa commercial area. <br /> <br />Reach 2: Location on the North Bank <br />characterized by low-to-moderate density <br /> <br />of the Rio <br />residential <br /> <br />Grande, it is <br />area with some <br /> <br />7 <br />