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<br />o <br />::; <br />N <br /> <br />CHAPTER I <br /> <br />GENERAL D ISCUSSIQ.NS <br /> <br />The remaining 21 percent of the water stored in Rifle Gap Res- <br />ervoir would be used for the irrigation of lands under Davie ditch, <br />Use of the ditch was discontinued several years ago because of the <br />inadequate water supply provided under its junior water right. Davie <br />ditch has deteriorated and VIOuld 'have to be completely reconstructed. <br />The new Davie ditch VIOuld head about 18 feet above dead Storage level <br />of the Rifle Gap Reservoir and 40 feet below the normal reservoir water <br />surface. A riser pipe from the outlet would supply the ditch When the <br />reservoir water level was high enough to cause gravity flow. At lower <br />reservoir stages the water would be lifted to the ditch by a hydraulic <br />turbine-driven pump. The .turbine would be propelled by water released <br />for lands in lower Rifle Creek Valley. <br /> <br />Although essentially an irriga~ion development, the Silt project <br />would provide some sedirrent control, enhance recreational development, <br />and .aid in fish and wildlife conservation. The project would have no <br />effect on municipal and industrial water supplies, navigation, Dr <br />stream pollution abatement. Hydroelectric power developae nt in c on- <br />nection with the project would be infeasible. There are no Indian <br />lands in the area. <br /> <br />The plan for the Silt project is correlated with a broad plan for <br />development of the land and water resources of the Upper Colorado <br />River Basin. The project is among the first developments recomnended <br />by States of the Upper Colorado River Basin for participation in the <br />benefits and revenues of the Colorado River Storage project, the master <br />project in the plan for upper basin development. Additiortal information <br />on the re lation of the project to the storage project is given in the <br />Bureau of Reclama Uon Report of December 1950, en titled Colorado River <br />Storage Pro~ect ~ Particfpating Pro~ects. <br /> <br />d~~ <br /> <br />Physical Geogra12hl <br /> <br />, <br />i <br />~. <br />~ <br />, <br />( <br /> <br />The project area is bound on the west by Rifle Creek, on the north <br />by the White River Plateau, on the east by Elk Creek, and on the south <br />by the Colorado River. The dominant structural features of the area, <br />Grand Hogback and \lhite River Plateau, are a result of thrust faulting. <br />Grand Hogback is in a zone of folding and falllting v.hich extends for <br />nearly 200 miles from Gunnison to north of Meeker. The hogback consists <br />of steeply dipping sandstone flanked on either side by easily eroded <br />shale. The hogback begins 30 miles south of Glenwood Springs and ex- <br />tends northward to be cut by the Colorado River at New Castle. From <br />her e it extends northwest acros s the pro ject ar ea, reaching elevations <br />of 9,000 feet. The narrow gorges where streams have pierced the hogback <br />make attractive dam and reservoir sites. TheYfuite River Plateau is a <br />Pfoduct of the uplift that formed the steep dips of Grand Hog'Dack at its <br />margin. The plateau, a: domal uplift 30 to 50 miles across, includes <br />headwaters of Rifle (:reek. <br /> <br />, <br /> <br />( <br /> <br />2 <br />