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INTRODUCTION <br />The Colorado River Basin drains portions of seven western <br />states (Wyoming, Colorado, Utah, Nevada, New Mexico, Arizona, and <br />California) and approximately 8% of the land surface area of the <br />United States (Bishop and Porcella 1980). It is unsurpassed as a <br />source of water for consumptive use, but has a very minor <br />discharge compared to that of eastern rivers (Pillsbury 1981). <br />To assist in the administration of water management programs, the <br />U.S. Congress divided the Basin into roughly equal upper and <br />lower segments in 1928 (Figure 1). f <br />The Upper Colorado River Basin, which extends 885 km from <br />north to south and 563 km from east to west, drains 283,600 km2 <br />in southwestern Wyoming, western Colorado, eastern Utah, <br />northwestern New Mexico, and northeastern Arizona. The primary <br />lotic systems of this section are the mainstem Colorado, Green, <br />Yampa, White, Gunnison, Dolores and San Juan rivers. Several <br />authors have further subdivided the Upper Basin into three major <br />hydrologic sub-basins: Upper Mainstem Colorado, Green, and San <br />Juan (Iorns et al. 1965, Joseph et al. 1977, Carlson and Carlson <br />1982). <br />The San Juan Sub-basin is the second largest of the Upper <br />Colorado River Basin subdivisions and drains 99,200 km2 in <br />Colorado, Utah, New Mexico, and Arizona. The primary riverine <br />components in this section are the Dirty Devil, Escalante, and