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the region primarily used for irrigation, are a major concern in Arkansas and Mississippi. <br />Water -level declines in the Mississippi River Valley Alluvial have changed the surface - <br />water /ground -water relationship resulting in a significant reduction of base flows in <br />streams. For example, typical base flow in the Sunflower River in Mississippi is only <br />about 10 percent of historical base flow. The Sparta aquifer and its equivalents have been <br />primary sources of high quality water for many industrial and municipal users throughout <br />Arkansas, Louisiana, Mississippi, and Tennessee. Continued pumping from the Sparta <br />aquifer since the 1920's has caused significant water -level declines in the region. Such <br />declines have resulted in the aquifer being declared "critical" in Arkansas and nominated <br />for "critical" status in Louisiana. Other areas in the region also are heavily dependent on <br />ground water for public supply and industrial purposes. For example, Memphis, <br />Tennessee and West Memphis, Arkansas is one of the largest metropolitan areas in the <br />world that relies exclusively on ground water for municipal supply. This heavy reliance <br />on ground water has resulted in interstate concerns over continued and increased <br />pumpage in the Memphis area. <br />9 Souris- Red -Rainy Region - -The Souris- Red -Rainy Region is located along the northern <br />boundary of the United States in Minnesota and North Dakota, and extends short <br />distances into South Dakota and Montana. The region drains northward into the Hudson <br />Bay of Canada. It consists of three basins: the Souris River on the west; Red River of the <br />North in the center; and Rainy River on the east. Continental glaciers left a poorly <br />drained landscape of broad, flat plains along the center of the region surrounded by <br />gently rolling uplands, lakes, potholes, and wetlands. Many areas do not contribute to <br />stream outflow, but comprise closed basins. Precipitation varies greatly across the region <br />resulting in average annual runoff that ranges from 0.2 inches in the western part of the <br />Souris to about 10 inches in the eastern part of the Rainy Basin. Ground water, derived <br />primarily from disconnected sand and gravel aquifers throughout the region and from <br />sedimentary rocks in the western part of the region, is sufficient to support rural water <br />supply and some irrigation of crops. Surface and ground water are sufficient for public <br />supply, light industrial uses and in the heavily forested Rainy Basin for recreational use. <br />Population growth of the region is most significant along the Red River of the North, <br />which is beginning to stress water availability from surface and ground waters. This <br />stress is raising the level of debate about the transfer of water from the Missouri River <br />and potential effects on downstream users regarding water quality and introduced biota. <br />10 Missouri River Region - -On the mainstem of the Missouri River, navigation interests <br />compete with environmental interests on the timing and amounts of water in the lower <br />river. In addition, recreational interests associated with large reservoirs in the upper basin <br />States contend with navigation interests in the lower basin States for water during <br />droughts. Recreational interests in the upper basin need stable water levels in reservoirs <br />and navigation interests need to draw down reservoirs to provide enough flow for <br />navigation downstream of Sioux City, IA. Several lawsuits are pending in the federal <br />courts on these issues. Numerous other water availability issues exist within this large <br />and diverse basin. The most visible ground -water issues are associated with the High <br />Plains aquifer, which occurs throughout the southern part of the basin. Extensive <br />19 <br />