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<br />c <br /> <br />,~~ <br />~ <br /> <br />...' <br /> <br />Needs for Further Development of Water and Related Land Resources <br /> <br /><: <br /> <br />the coal is processed locally for thermal electric generation or coal gasifi- <br />cation, or if it is transported by slurry pipeline, the water requirements <br />would be significant. <br /> <br />Future needs for municipal water cannot be reasonably predicted without more <br />definitive and supportive predictions from the oil shale and coal industries. <br /> <br />Flood Control Needs <br /> <br />Flood damages in the basin have been minor because of the low population <br />density and lack of urban and residential development in the flood plain. <br />Two distinct types of floods occur in the Yampa basin, the spring snowmelt <br />floods and .the summer thunderstorm floods. The first type is caused by <br />rapid snowmelt in the early spring which produces large volumes of water <br />over a period of several days or a week. Many of the streams near the head- <br />waters of the basin are not deeply entrenched and the normal springtime <br />flows spread out over considerable bottom or floodplain areas. Since this <br />is a normal annual occurrence, very little development has occurred on these <br />floodplains. The farmers utilize these areas as wet meadows or pastures, or <br />as feeding grounds during the winter. Occasionally, ice jams will increase <br />the area of flooding and damage. These spring snowmelt floods can cause <br />streambank erosion, damage to diversion structures, erosion of low lying <br />fields and delay in crop growth. <br /> <br />The second type of flood is caused by summer thunderstorms which tend to <br />produce flash floods in localized areas with high peak flows with low total <br />volumes of water. These floods can result in local damage to cropland and <br />other land and to improvements such as roads, bridges, irrigation structures, <br />and other facilities. Large volumes of mud and debris may be carried by <br />these floods and deposited in headgates, culverts, roads, and fields. <br /> <br />Historically, major floods have occurred on Fortification Creek which flows <br />through Craig, Colorado. These floods resulted from snowmelt or a combina- <br />tion of snowmelt and rainfall. Ice jams at creek obstructions in the town <br />of Craig have caused some of the flooding. Some channelization under the <br />direction of the U.S. Army Corps of Engineers has been done to provide for <br />better flow conditions through Craig. The town of Craig has had consider- <br />able urban expansion on the Fortification Creek floodplains in recent years, <br />and potential damage from even minor overflows would now be extensive. <br /> <br />A total of approximately 42,900 acres in the Yampa River basin are subject <br />to floodwater and sediment damage. Of this total acreage, 700 acres are <br />within urban areas and the remaining 42,200 acres are agricultural lands. <br />All of the urban areas and most of the agricultural lands subject to flood <br />damage are located upstream from Cross Mountain Canyon. <br /> <br />. <br />Several areas of irrigated land in the basin, in particular those along the <br />main tributaries, are being eroded away during high stream flows. <br /> <br />20 <br />