Hydrogeologic framework of the North Carolina Coastal Plain aquifer system
Open-File Report
87-690
By: M. D. Winner Jr. and R. W. Coble
Links
- Document: Report (pdf)
- Plates:
- Plate 1 (pdf)
- Plate 2 (pdf)
- Plate 3 (pdf)
- Plate 4 (pdf)
- Plate 5 (pdf)
- Plate 6 (pdf)
- Plate 7 (pdf)
- Plate 8 (pdf)
- Plate 9 (pdf)
- Plate 10 (pdf)
- Plate 11 (pdf)
- Plate 12 (pdf)
- Plate 13 (pdf)
- Plate 14 (pdf)
- Plate 15 (pdf)
- Plate 16 (pdf)
- Plate 17 (pdf)
- Plate 18 (pdf)
- Plate 19 (pdf)
- Plate 20 (pdf)
- Plate 21 (pdf)
- Plate 22 (pdf)
- Plate 23 (pdf)
- Plate 24 (pdf)
- Plate 25 (pdf)
- Plate 26 (pdf)
- Plate 27 (pdf)
- Plate 28 (pdf)
- Plate 29 (pdf)
- Plate 30 (pdf)
- Plate 31 (pdf)
- Plate 32 (pdf)
- Plate 33 (pdf)
- Plate 34 (pdf)
- Plate 35 (pdf)
- Plate 36 (pdf)
- Plate 37 (pdf)
- Plate 38 (pdf)
- Plate 39 (pdf)
- Plate 40 (pdf)
- Plate 41 (pdf)
- Plate 42 (pdf)
- Plate 43 (pdf)
- Plate 44 (pdf)
- Superseding Publications:
- Download citation as: RIS | Dublin Core
Abstract
The hydrogeologic framework of the North Carolina Coastal Plain aquifer system consists of ten aquifers separated by nine confining units. From top to bottom the aquifers are: the surficial aquifer, Yorktown aquifer, Pungo River aquifer, Castle Hayne aquifer, Beaufort aquifer, Peedee aquifer, Black Creek aquifer, upper Cape Fear aquifer, lower Cape Fear aquifer, and the Lower Cretaceous aquifer. The uppermost aquifer (the surficial aquifer in most places) is a water-table aquifer and the bottom of the system is underlain by crystalline bedrock. The sedimentary deposits forming the aquifers are of Holocene to Cretaceous age and are composed mostly of sand with lesser amounts of gravel and limestone. Confining units between aquifers are composed primarily of clay and silt. The thickness of the aquifers ranges from zero along the Fall Line to more than 10,000 feet at Cape Hatteras. Prominent structural features are the increasing easterly homoclinal dip of the sediments and the Cape Fear arch, the axis of which trends in a southeast direction. The stratigraphic continuity is determined from correlations of 161 geophysical logs along with data from drillers' and geologists' logs. Aquifers were defined by means of these logs plus water-level and water-quality data and evidence of the continuity of pumping effects. Eighteen hydrogeologic sections depict the correlation of these aquifers throughout the Coastal Plain.
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Hydrogeologic framework of the North Carolina Coastal Plain aquifer system |
| Series title | Open-File Report |
| Series number | 87-690 |
| DOI | 10.3133/ofr87690 |
| Year Published | 1989 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Publisher location | Reston, VA |
| Contributing office(s) | South Atlantic Water Science Center |
| Description | Report: x, 155 p.; 44 Plates: 52.15 x 23.77 inches or smaller |
| Country | United States |
| State | North Carolina |
| Other Geospatial | North Carolina Coastal Plain aquifer system |
| Google Analytic Metrics | Metrics page |