Regional hydrology and simulation of deep ground-water flow in the Southeastern Coastal Plain aquifer system in Mississippi, Alabama, Georgia, and South Carolina
Professional Paper
1410-C
By: R.A. Barker and Maribeth Pernik
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Abstract
The Southeastern Coastal Plain aquifer system is a coastward-sloping, wedge-shaped sand and gravel reservoir exposed in outcrop to a humid climate and drained by an extensive surface-water network. Ground-water pumpage has increased to about 765 cubic feet per second since 1900, causing water-level declines of more than 150 feet in places, while base flow to major streams has decreased about 350 cubic feet per second. The water-level declines and adjustments in recharge and discharge are not expected to seriously restrict future ground-water development.
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Regional hydrology and simulation of deep ground-water flow in the Southeastern Coastal Plain aquifer system in Mississippi, Alabama, Georgia, and South Carolina |
| Series title | Professional Paper |
| Series number | 1410 |
| Chapter | C |
| DOI | 10.3133/pp1410C |
| Edition | - |
| Year Published | 1994 |
| Language | ENGLISH |
| Contributing office(s) | South Atlantic Water Science Center |
| Description | p. C1-C87; 10 plates in separate case |
| Country | United States |
| State | Alabama, Florida, Georgia, Mississippi, South Carolina |
| Online Only (Y/N) | N |
| Additional Online Files (Y/N) | N |
| Google Analytic Metrics | Metrics page |