Hydrology Of The Manokin, Ocean City, And Pocomoke Aquifers Of Southeastern Delaware
| Author(s) | Hodges, A.L. Jr. | |
| Date Accessioned | 2008-03-28T19:25:51Z | |
| Date Available | 2008-03-28T19:25:51Z | |
| Publication Date | 1984-01 | |
| Abstract | Population and accompanying water use are expected to increase by 34 percent in southeastern Delaware between 1975 and 2000. To assess the capability of the aquifers in that area to supply the required amount of ground water, a study of those aquifers was started in 1976. Interpretation of geologic sections developed from drilling and geophysical data showed that the confining beds between the Manokin, Ocean City, and Pocomoke aquifers of Neogene age are thin and discontinuous in some parts of the area. Possible fault zones coinciding with deep tectonic features may also contribute to interconnection of these aquifers. Hydrographs of water levels in the aquifers show differential drawdown during periods of heavy pumping, but levels return to a common altitude during unstressed periods. Because of these characteristics, the Manokin, Ocean City, and Pocomoke aquifers are considered to be a single confined aquifer, in most places. | en_US |
| Sponsor | Prepared under the Cooperative Program of the Delaware Geological Survey and the United States Geological Survey. | en_US |
| URL | http://udspace.udel.edu/handle/19716/3151 | |
| Language | en_US | en_US |
| Publisher | Newark, DE: Delaware Geological Survey, University of Delaware | en_US |
| Part of Series | Report of Investigations | en_US |
| Part of Series | 38 | en_US |
| Keywords | southeastern Delaware water use | en_US |
| Keywords | Manokin aquifer | en_US |
| Keywords | Pocomoke aquifer | en_US |
| Keywords | Ocean City aquifer | en_US |
| Title | Hydrology Of The Manokin, Ocean City, And Pocomoke Aquifers Of Southeastern Delaware | en_US |
| Type | Technical Report | en_US |