Saturated Thickness of the Water-Table Aquifer in Southern New Castle County, Delaware
| Author(s) | Groot, J.J. | |
| Author(s) | Demicco, P.M. | |
| Author(s) | Cherry, P.J. | |
| Date Accessioned | 2008-05-30T19:13:34Z | |
| Date Available | 2008-05-30T19:13:34Z | |
| Publication Date | 1983 | |
| Abstract | This map shows the saturated thickness of the water-table aquifer. This aquifer consists of the deposits of the Columbia Formation and those portions of the Magothy and Englishtown-Mt. Laurel formations, and Rancocas Group that are hydraulically connected with the Columbia deposits (see Groot, Demicco, and Cherry, 1983). For example, large, saturated thicknesses in the zone trending northeast-southwest near Townsend reflect the addition of the sands of the Rancocas Group to the total thickness of the sands of the overlying Columbia Formation. | en_US |
| URL | http://udspace.udel.edu/handle/19716/3232 | |
| Language | en_US | en_US |
| Publisher | Newark, DE: Delaware Geological Survey, University of Delaware | en_US |
| Part of Series | Open File Report | en_US |
| Part of Series | 24 | en_US |
| Keywords | water-table aquifer | en_US |
| Keywords | Columbia Formation | en_US |
| Keywords | Magothy Formation | en_US |
| Keywords | Englishtown-Mt. Laurel Formation | en_US |
| Keywords | Rancocas Group | en_US |
| Title | Saturated Thickness of the Water-Table Aquifer in Southern New Castle County, Delaware | en_US |
| Type | Map | en_US |