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in the region, the absence of large river basins has resulted in increasing and often <br />controversial interbasin transfers to meet water - supply needs. Across the region, public <br />supply withdrawals are split almost equally between surface and ground water. There <br />are, however, large differences among States in the region. Florida, for example, <br />withdraws about 90 percent of its public water supply from the ground -water system, <br />whereas Georgia, North Carolina, and South Carolina all utilize surface water for about <br />80 percent of their public water supplies. About 20 percent of the population in the <br />region relies on private ground -water systems for water supply. Heavy ground -water <br />pumping in many areas of the region, particularly in the Coastal Plain, has resulted in the <br />loss of wetlands, disappearance of lakes, land subsidence, and saltwater intrusion into <br />coastal aquifers. The presence of karst formations throughout much of the region and <br />intensive agricultural operations in other areas means that shallow ground -water systems <br />are highly susceptible to contamination. Aquifer storage and recovery is increasingly <br />seen as a method for storing water supplies in the Coastal Plain where topography <br />prevents the construction of large reservoirs, and several large cities are considering <br />desalinization. <br />4 Great Lakes Region - -The Great Lakes Region includes parts of eight States and two <br />Canadian Provinces and contains a reservoir of fresh surface water that is 18 percent of <br />the world's supply and 95 percent of North America's supply. Even though the resource <br />is vast, uncertainties in the estimates of the water inflows, outflows, and water use in the <br />Great Lakes Basin threatens the ability of the States to provide defensible decision <br />making under Annex 2001 to the Great Lakes Charter. In particular, improvements are <br />needed in the computations of tributary and connecting channel streamflow, ground- <br />water contributions, and consumptive uses. Some water withdrawals may be negligible <br />compared to the total amount of water in the Great Lakes, but they may be large relative <br />to the tributary stream or ground -water reservoir from which they are withdrawn. <br />5 Ohio Region - -The Ohio Region includes most of Indiana, Kentucky, Ohio, West <br />Virginia, and small portions of seven other States. The region on average is water rich, <br />accounting for one third of the annual outflow of the Mississippi River. Although the <br />resource especially along the major river systems is large, surface- and ground -water <br />availability in many areas can be limited by lower natural storage and flow characteristics <br />or by a lack of supply development and infrastucture. Surface -water systems are a much <br />more common source of public -water supply than are ground -water systems, especially in <br />the bedrock dominated portions of the region. Exceptions, however, include the alluvial <br />and glacial outwash aquifers bordering the major rivers where large quantities of ground <br />water are pumped from the sand and gravel deposits and used for public and industrial <br />water supplies. A rapidly growing portion of the population is expanding into suburban <br />and rural areas. These areas tend to be more dependent upon the use of local surface- and <br />ground -water systems that often are less reliable during drought conditions and prone to <br />contamination. One distinguishing characteristic of the region is the large proportion of <br />karst (mostly limestone) terrain whose hydrologic complexity has not yet been <br />quantitatively well defined. <br />17 <br />