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25 percent population increase in the Colorado Front Range urban corridor illustrates the growth <br />which necessitates better water resources planning. <br />The economy in the mountainous headwaters area of the South Platte River basin is based on <br />tourism and recreation, while the economy in the urbanized south-central region is related mostly <br />to manufacturing, service and trade industries, and government services. The economy of the <br />basin downstream from Denver is based primarily on agriculture and livestock production. <br />Agriculture is the predominant water use in the South Platte River basin. Approximately <br />2.0 million acre-feet per year of surface water are used for irrigation of approximately 1.1 million <br />acres (Colorado Division of Water Resources 1994 and 1998a). Average annual flow of the <br />South Platte River at Julesburg Colorado is approximately 394,000 acre-feet, thereby indicating <br />that South Platte River water is used and reused several times within Colorado before it leaves <br />the State (Colorado Water Conservation Board 2000). <br />1.2.2 North Platte River Basin <br />The North Platte River basin (see Figure 1-1) drains the north-central portion of Colorado and <br />consists of the North Platte River and two tributaries, the Laramie River and Sand Creek, which <br />originate in Colorado and join the North Platte River in Wyoming. The Michigan, Illinois and <br />Canadian Rivers, and Grizzly Creek are tributaries to the North Platte River in Colorado. This <br />basin is comprised of portions of Larimer and Jackson counties with the majority of the <br />population in Jackson County, which had a 1999 population of 1,810 (Colorado Department of <br />Local Affairs 2001). <br />Water use is controlled by U.S. Supreme Court decrees for the North Platte and Laramie Rivers. <br />The major water use in the North Platte River basin is for irrigation of approximately <br />120,900 acres of agricultural land (Colorado Division of Water Resources 1998b). <br />1.2.3 Hydrogeologic Conditions in the South Platte River Basin <br />The South Platte River basin groundwater system consists of multiple aquifers including the <br />South Platte alluvium, the Denver Basin system and several Designated Groundwater Basins. <br />A "Designated Groundwater Basin" means the area established by the Colorado Groundwater <br />Commission in accordance with Section 37-90-106 of the Colorado Revised Statutes. There are <br />seven Designated Groundwater Basins including Upper Crow Creek, Northern High Plains, Lost <br />Creek, Kiowa-Bijou, Upper Big Sandy, Upper Black Squirrel Creek and Southern High Plains. <br />Recharge for these basins comes from precipitation and seasonally from streams. <br />The alluvial aquifer along the South Platte River downstream from Denver and its tributaries can <br />vary in width from 1 to 10 miles and from 5 to 200 feet in thickness. An estimated 8.3 million <br />acre-feet of water is contained in the South Platte alluvium (Hurr et al. 1975). This aquifer is <br />recharged through precipitation, irrigation return flows, canal seepage, and seasonally from flows <br />p:data\gen\spdss\final report\chapter l.doc 1-4 <br />October 31, 2001 <br />