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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Both types at tributaries, as well as the South Platte River itself, <br /> <br /> <br />exhibit substantial variations in streamflow from season to season and from <br /> <br /> <br />year to year. Characteristically, as much as 75 percent of the runoff of <br /> <br /> <br />mountain streams may occur during the months of May through July. In <br /> <br />tributary sub-basins of the Plains zone, summer thunderstorms may result in <br /> <br /> <br />relatively large streamflows during July, August, or September. On a <br /> <br />relative basis, substantially larger annual streamflow volumes per unit <br /> <br /> <br />area are generated in the mountains than in the plains. These pronounced <br /> <br /> <br />seasonal and Ioeational variations suggest the need for water storage <br /> <br /> <br />projects for water uses requiring sustained yields or year-round supplies. <br /> <br />The reach of the South Platte River extending from about Henderson <br /> <br /> <br />downstream is underlain by valley-fill alluvium and dune sand containing an <br /> <br /> <br />unconfined aquifer. This aquifer varies in width from about 1 mile to over <br /> <br /> <br />10 miles; generally, it is narrowest downstream from Sterling and widest <br /> <br /> <br />immediately above Fort Morgan where Kiowa and Bijou Creeks discharge into <br /> <br />the SOuth Platte River (Figure 8). The aquifer is estimated to contain as <br /> <br /> <br />much as 8 million acre-feet of water in storage and is connected to the <br /> <br /> <br />surface flow of the river (Hurr and others, 1975). Upstream from <br /> <br />Henderson, the valley-fill aquifer is limited in size and storage <br /> <br /> <br />capabilities. <br /> <br />Transbasin diversion projects have delivered a significant amount of water <br /> <br /> <br />into the South Platte River basin from Colorado's western slope and the <br /> <br /> <br />Laramie River basin. This water, averaging nearly 377,000 acre-feet <br /> <br /> <br />annually over the 1953-79 water year period, has been used for <br /> <br /> <br />agricultural, municipal and industrial purposes. Notable examples of <br /> <br /> <br />tranebasin-import projects are the Moffat collection system and the Blue <br /> <br />River system operated by the Denver Water Board, and the Colorado-Big <br /> <br /> <br />Thompson Project, operated by the u.s. Bureau of Reclamation and the <br /> <br /> <br />Northern Colorado Water Conservancy District. The significant transbasin <br /> <br />import projects are discussed later. <br /> <br />-27- <br />