Reliable and impartial scientific information about the occurrence, quantity, quality, distribution, and movement of water is essential to resource managers, planners, and others throughout the Nation. The U.S. Geological Survey (USGS), in cooperation with numerous local, State, and Federal agencies, collects hydrologic data and conducts studies to monitor hydrologic conditions and better define the water resources of Georgia and other States and territories.
Groundwater-level and groundwater-quality data are essential for water-resources assessment and management. Water-level measurements from observation wells are the principal source of information about the hydrologic stresses on aquifers and how these stresses affect groundwater recharge, storage, and discharge. Long-term, systematic measurement of water levels provides essential data needed to evaluate changes over time, develop groundwater models, forecast trends, and design, implement, and monitor the effectiveness of groundwater management and protection programs (Taylor and Alley, 2001). Groundwater-quality data are necessary to protect groundwater resources, because deterioration of groundwater quality may be virtually irreversible, and treatment of contaminated groundwater can be expensive (Alley, 1993).
Purpose and Scope
This website presents an overview of groundwater levels throughout Georgia. It is a continuation of a series of reports begun in 1978. Water-level data are summarized in graphs and maps. Groundwater levels in major aquifers are presented on hydrographs for selected wells. Data from additional information about the wells included in this report can be obtained from the USGS National Water Information System (NWIS) database at http://waterdata.usgs.gov/ga/nwis/gw/.
Cooperating Organizations and Agencies
Groundwater monitoring in Georgia is conducted in cooperation with numerous local organizations, private companies, and State and Federal agencies. Cooperating organizations and agencies include the following:
- City of Albany Utility Operations
- Augusta Utilities Department, City of Augusta
- Georgia Department of Natural Resources, Environmental Protection Division
- Glynn County Joint Water and Sewer Commission
- Miller Coors LLC
All of these organizations participate in USGS Cooperative Matching Funds (CMF) which support joint projects with our state, regional, tribal, and local partners to provide reliable, impartial, and timely information needed to understand and manage the Nation's water resources. A more complete description of the CMF is provided in on the USGS Cooperative Matching Funds website: https://www.usgs.gov/mission-areas/water-resources/science/usgs-cooperative-matching-funds?qt-science_center_objects=0#qt-science_center_objects (USGS, accessed June 9, 2020).
Linear Trend Lines and Regression Statistics
Water-level trend lines are generated by Simple Linear Regression. The "Simple Regression" button calculates the trend line for the current set of data displayed in the graph.
Dates with null values are not used in the trend line calculations.
η represents the sample size
y-intercept a = [ (∑y)(∑x2) - (∑x)(∑xy) ] / [ η(∑x2) - (∑x)2 ]
slope b = [ η(∑xy) - (∑x)(∑xy) ] / [ η(∑x2) - (∑x)2 ]
Arrow icons for the maps represent the upward or downward trend, and are calculated using the last 10 years of data. Simple Linear Regression is used to calculate the trend. If the well does not have 10 years of data, or if the trend is less than .01 ft/year, a circle icon is displayed, instead of an arrow.
Methods of Analysis, Sources of Data, and Data Accuracy
Continuous water-level data from wells throughout Georgia are presented in this report. Wells with electronic data loggers record water levels at 15-minute intervals; these data are field checked to verify that the electronic water level is within 0.05 foot (ft) of the manual measurement, and data are retrieved generally every 2 months. Wells that have real-time satellite telemetry record water levels at 15-minute intervals and are transmitted every 1 to 4 hours (based on the equipment). The data are available at https://waterdata.usgs.gov/ga/nwis/current/?type=gw.
Vertical coordinate information is referenced to the North American Vertical Datum of 1988 (NAVD 88) or National Geodetic Vertical Datum of 1929. Horizontal coordinate information is referenced to the North American Datum of 1983 (NAD 83) or North American Datum of 1927 (NAD 27). The datum information for each site are available at https://waterdata.usgs.gov/ga/nwis/current/?type=gw.
Altitude, as used in this report, refers to distance above the vertical datum.
Contrasting geologic features and landforms of the physiographic provinces of Georgia (see map above) affect the quantity and quality of groundwater throughout the State. The surficial aquifer system is present in each of the five physiographic provinces in Georgia. In the Coastal Plain Province, the surficial aquifer system consists of layered sand, clay, and in some places limestone. The surficial aquifer system typically is under water-table (unconfined) conditions and provides water for domestic and livestock use. The surficial aquifer system is semiconfined to confined locally in the coastal area. In the Piedmont, Blue Ridge, and Valley and Ridge Provinces, the surficial aquifer system consists of soil, saprolite, stream alluvium, colluvium, and other surficial deposits.
The most productive aquifers in Georgia are in the Coastal Plain Province in the southern half of the State. The Coastal Plain is underlain by alternating layers of sand, clay, dolomite, and limestone that dip and thicken to the southeast. Coastal Plain aquifers generally are confined, except near their northern limits where the aquifers crop out or are near land surface. Aquifers in the Coastal Plain include the surficial aquifer system, Brunswick aquifer system, Floridan aquifer system, Gordon aquifer, Claiborne aquifer, Clayton aquifer, and Cretaceous aquifer system.
In the Valley and Ridge Province, groundwater is transmitted through primary and secondary openings in folded and faulted sedimentary and metasedimentary rocks of Paleozoic age. In this report, the aquifers are referred to as “Paleozoic-rock aquifers.”
In the Piedmont and Blue Ridge Provinces, the geology is complex and consists of structurally deformed metamorphic and igneous rocks. Groundwater is transmitted through secondary openings along fractures, foliation, joints, contacts, or other features in the crystalline bedrock. In this report, the aquifers are referred to as “crystalline-rock aquifers.” A more complete discussion of the State’s groundwater resources is provided in Clarke and Pierce (1985).
- Alley, W.M., 1993, General design consideration, in Alley, W.M., ed., Regional groundwater quality: New York, Van Nostrand Reinhold, 634 p.
- Clarke, J.S., 2003, The surficial and Brunswick aquifer systems—Alternative groundwater resources for coastal Georgia, in Hatcher, K.J., ed., Proceedings of the 2003 Georgia Water Resources Conference, April 23–24, 2003: Athens, Georgia, University of Georgia, https://smartech.gatech.edu/handle/1853/48399.
- Clarke, J.S., Brooks, Rebekah, and Faye, R.E., 1985, Hydrology of the Dublin and Midville aquifer system of east-central Georgia: Georgia Geologic Survey Information Circular 74, 62 p, https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/IC-74.pdf
- Clarke, J.S., Faye, R.E., and Brooks, Rebekah, 1983, Hydrogeology of the Providence aquifer of southwest Georgia: Georgia Geologic Survey Hydrologic Atlas 11, 5 sheets, https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/HA-11.pdf
- Clarke, J.S., Hacke, C.M., and Peck, M.F., 1990, Geology and groundwater resources of the coastal area of Georgia: Georgia Geologic Survey Bulletin 113, 106 p, https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/B-113.pdf
- Clarke, J.S., and Pierce, R.R., 1985, Georgia groundwater resources, in U.S. Geological Survey, National Water Summary, 1984: U.S. Geological Survey Water-Supply Paper 2275, p. 179–184, https://pubs.er.usgs.gov/publication/wsp2275
- Cressler, C.W., 1964, Geology and groundwater resources of Walker County, Georgia: Georgia Geologic Survey Information Circular 29, 15 p, https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/IC-29.pdf
- Cressler, C.W., Thurmond, C.J., and Hester, W.G., 1983, Groundwater in the greater Atlanta region, Georgia: Georgia Geologic Survey Information Circular 63, 144 p, https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/IC-63.pdf
- Gordon, D.W., Peck, M.F., and Painter, J.A., 2012, Hydrologic and water-quality conditions in the lower Apalachicola–Chattahoochee–Flint and parts of the Aucilla–Suwanee–Ochlockonee River basins in Georgia and adjacent parts of Florida and Alabama during drought conditions, July 2011: U.S. Geological Survey Scientific Investigations Report 2012–5179, 69 p., 1 sheet, available online at http://pubs.usgs.gov/sir/2012/5179/.
- Hicks, D.W., Krause, R.E., and Clarke, J.S., 1981, Geohydrology of the Albany area, Georgia: Georgia Geologic Survey Information Circular 57, 31 p, https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/IC-57.pdf
- Jones, L.E., and Maslia, M.L., 1994, Selected groundwater data, and results of aquifer tests for the Upper Floridan aquifer, Brunswick, Glynn County, Georgia, area: U.S. Geological Survey Open-File Report 94–520, 107 p, https://pubs.er.usgs.gov/publication/ofr94520
- Krause, R.E., and Randolph, R.B., 1989, Hydrogeology of the Floridan aquifer system in southeast Georgia and adjacent parts of Florida and South Carolina: U.S. Geological Survey Professional Paper 1403–D, 65 p, https://pubs.er.usgs.gov/publication/pp1403D
- National Weather Service, Climate Prediction Center, Drought Monitoring, accessed June 9, 2020 at URL https://www.cpc.ncep.noaa.gov/products/monitoring_and_data/drought.shtml
- Painter, J.A., 2019, Estimated use of water in Georgia for 2015 and water-use trends, 1985–2015: U.S. Geological Survey Open-File Report 2019–1086, 216 p, https://doi.org/10.3133/ofr20191086
- Peck, M.F., Joiner, C.N., and Cressler, A.M., 1992, Groundwater conditions in Georgia, 1991: U.S. Geological Survey Open-File Report 92–470, 137 p, https://pubs.er.usgs.gov/publication/ofr92470
- Peck, M.F., McFadden, K.W., and Leeth, D.C., 2005, Effects of decreased ground-water withdrawal on ground-water levels and chloride concentrations in Camden County, Georgia, and ground-water levels in Nassau County, Florida, from September 2001 to May 2003: U.S. Geological Survey Scientific Investigations Report 2004–5295, 36 p., accessed August 24, 2016, at https://pubs.usgs.gov/sir/2004/5295
- Pollard, L.D. and Vorhis, R.C., 1980, The geohydrology of the Cretaceous aquifer system in Georgia: Georgia Geologic Survey Hydrologic Atlas 3, 5 sheets, at https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/HA-3.pdf.
- Taylor, C.J., and Alley, W.M., 2001, Groundwater-level monitoring and the importance of long-term water-level data: U.S. Geological Circular 1217, 68 p., accessed May 15, 2018, at https://pubs.usgs.gov/circ/circ1217/.
- U.S. Geological Survey, USGS Cooperative Matching, accessed June 9, 2020 at URL https://www.usgs.gov/mission-areas/water-resources/science/usgs-cooperative-matching-funds?qt-science_center_objects=0#qt-science_center_objects