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<br />,I' <br /> <br />or10115," <br /> <br />"1' <br />,'.,..,' <br /> <br />}' <br />,- <br />i <br /> <br />," <br /> <br />WATER SUPPLY AND DEPLETIONS OF THE SAN JUAN RIVER IN COlDRAOO <br /> <br />I. Introduction <br /> <br /> <br />The purpose of this report is to evaluate the effect of the <br /> <br /> <br />man-made depletions, both present and future, on the water supply <br /> <br /> <br />of the San Juan River and its tributaries in Colorado. The San <br /> <br />Juan River, which joins the Colorado River in southern Utah, is <br />the second largest tributary of the Colorado River, furnishing <br />20 percent of the flow of the Colorado River at Lee's Ferry. <br />The source of the water supply of the San Juan River is primarily <br />in the mountains of southwestern Colorado. <br />The tributary areas of the San Juan can be classified according <br />to sub-basins. The easternmost of these sub-basins is the Upper <br />San Juan Basin which includes such tributaries as the Navajo River, <br />the Rio Blanoo, the East Fork of the San Juan River, the West <br />Fork of the San Juan, and numerous smaller streams. The sub- <br />basins to the west are named by the main streams that traverse <br />the basins. These include the Piedra River Basin, the Los Pinos <br />River Basin, the Florida and Animas Rivers Basins, the La Plata <br />River Basin, the Mancos River Basin, and the McElmo Creek drain- <br />age area. The McElmo Creek watershed drains into Utah before <br />joining the San Juan River. <br />Future developments of the water supply of the San Juan River <br />will deplete the flow at the state line. This report attempts to <br />evaluate these depletions and their effect on the historic flow <br />that would occure during a dry period, su~h as 1934 and through <br /> <br />1954. <br /> <br />- <br />The Dolores Project will increase the flow of the San Juan <br />" <br /> <br /> <br />River because the diversion will be from the Dolores River to lands <br /> <br />. ...L. ; ,._~. <br />