USGS  

Ground-Water Resources and Hydrogeology of Crystalline-Rock Aquifers in Rockdale County

Cooperator: Rockdale County
Year Started: 2001

Photo 
showing a jointed granite gneiss located along
Highway 138 approximately 2.5 miles north of the International
Horse Park. The jointed granite gniess exhibits
well developed fracture openings that parallel gneissic
layering. Photo by Ethan W. Williams.

Until recently, it was widely accepted that little ground water was available from crystalline-rock aquifers of the Piedmont, and hence ground water was largely ignored as a viable water resource. Although ground water in the Piedmont may never be developed as a sole-source for a large municipality, this resource has been developed successfully as a dependable supplemental source for existing water supplies. If properly developed and managed, supplemental use of ground water can have great economic, environmental, and other practical benefits. Rockdale County is a high-growth area that plans to evaluate alternative sources of water to its existing surface-water supply. The county previously operated five wells that tapped into a productive granite gneiss unit; however, these wells are no longer used.

The U.S. Geological Survey (USGS), in cooperation with Rockdale County, is evaluating ground-water availability and quality in crystalline-rock aquifers that underlie the area. Information from this project will be used for development of water resources. In addition, the ground-water studies in Rockdale County will allow the USGS to compile detailed information on rock types and geologic structures that tend to promote development of high-yielding waterbearing fractures. This information will help foster a better understanding of these aquifers and provide information for the future development and management of this resource.


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Last updated Monday, 09-Jun-2003 15:20:48 EDT
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