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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 />EXECUTIVE SUMMARY <br /> <br />Introduction <br /> <br />This report summarizes the results of Phase One of the San Miguel study for review by the study participants and <br />by the public. This study was authorized by the Colorado Legislature in HB 1042 of the 1985 session and is <br />sponsored by the San Miguel Water Conservancy District (SMWCD) and the Colorado Water Conservation <br />Board (CWCB). The objective of the study is to investigate several alternatives for improving and expanding the <br />existing irrigation systems located in the SMWCD area. <br /> <br />Studv Area <br /> <br />The study area is located in San Miguel and Montrose counties of southwestern Colorado on the south side of the <br />San Miguel River generally between Placerville and Naturita. Surface drainage in the study area is provided by a <br />system of streams which flow generally from southwest to northwest and into the San Miguel River. The major <br />tributaries to the San Miguel are, from downstream to upstream, Naturita Creek, Beaver Creek, Saltado Creek <br />and Fall Creek, <br /> <br />Irrigated agriculture has been practiced in the study area since the late 1800's. Currently, the area is served by <br />three major ditch companies; the Farmers' Water Development Company (which operates the Gurley System) <br />serving the Norwood-Redvale area; the Lone Cone Ditch and Reservoir Company serving the Norwood area; and <br />the Lilylands Canal and Reservoir Company serving the East Lilylands and Dry Creek areas, In addition, the <br />privately owned J & M Hughes Ditch serves irrigated pastureland on Beaver Mesa. <br /> <br />Water Availability and Water Demands <br /> <br />The two basic sources of water available for growing crops in the San Miguel study area are natural precipitation <br />and streamflow diverted for irrigation. Precipitation depths over the study area are low. Irrigation water is <br />supplied by diverting streamflow produced by snowmelt runoff from the mountains to the south. Streamflows are <br />high in the spring but low in the summer when crop water demands are high. Additional water supplies for <br />irrigation are needed in the late summer months, <br /> <br />v <br />