| Abstract: | The Coastal Plain aquifers are recharged primarily by precipitation in their outcrop areas. Groundwater flows from these areas of recharge, through the aquifers, and discharges to upper Costal Plain rivers, overlying aquifers as upward leakage, and wells. Ground-water flow in the Floridan aquifer system and the Tertiary sand aquifer prior to development is generally perpendicular to the coast.-from Authors |
| Genre: | Article |
| ProdID: | 70012763 |
| Citation Author: | Aucott, W. R.; Speiran, G. K. |
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| Citation End Page: | 745 |
| Citation Issue: | 6 |
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| Citation Language: | English |
| Citation Larger Work Title: | Ground Water |
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| Citation Number Of Pages: | 10 |
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| Citation Search Results Text: | Ground-water flow in the Coastal Plain aquifers of South Carolina.; 1985; Article; Journal; Ground Water; Aucott, W. R.; Speiran, G. K. |
| Citation Start Page: | 736 |
| Citation Volume: | 23 |
| Citation Year: | 1985 |
| Type: | citation/reference |
| Text: | Ground-water flow in the Coastal Plain aquifers of South Carolina.; 1985; Article; Journal; Ground Water; Aucott, W. R.; Speiran, G. K. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1985 00:00 -0600 |
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