USGS Open-File Report 00-515
Claiborne Aquifer
The water level in the Claiborne aquifer was monitored in 12 wells in 1999 and data from these wells are available as PDF files, accessible by clicking on the well number in the map below or from Table 3b. The water level in the aquifer is affected mainly by precipitation and by local and regional pumping (Hicks and others, 1981). The water level is generally highest following the winter and spring rainy seasons, and lowest in the fall following the summer irrigation season.
Figure 101. Location of observation wells completed in the Claiborne aquifer.
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Last updated Monday, 26-Jun-2000 15:14:17 EDT
The URL for this page is http://ga.water.usgs.gov/publications/ofr00-151/claib.html