Data and Graphs of Water Level Summaries for Wells with 20+ Years or 100+ Observations
Ground-water levels are basic information needed for evaluating water conditions and for basic and applied research. For these efforts, water levels are being measured statewide in wells completed in multiple aquifers. Some wells are measured for specific projects, such as the Coastal Aquifers Salinity Project and the Water Conditions program, while other wells are measured so that staff can maintain long term records of ground-water levels for evaluation of trends. Table contains summary data from wells having 100 or more water level observations.
- aquifer
- Cheswold aquifer
- Cockeysville aquifer
- Columbia aquifer
- Delaware
- Federalsburg aquifer
- Frederica aquifer
- groundwater
- instrumented borehole
- Kent County
- Magothy aquifer
- Manokin aquifer
- Mount Laurel aquifer
- New Castle County
- Piney Point aquifer
- Pocomoke aquifer
- Potomac aquifer
- Rancocas aquifer
- Sussex County
- TAB
- wells
- Wissahickon aquifer
- Interactive
RI46 Shallow Subsurface Temperatures at Selected Locations in Delaware
Subsurface temperatures were measured in instrumented boreholes for about one and one-half years at depths down to 10 feet below land surface at four locations in the State. In New Castle County, temperatures were measured periodically in the field about twice a month at three sites, and, in Sussex County, they were automatically recorded every 15 minutes at one site. The depths of interest are generally in the unsaturated zone and are subject to both daily temperature fluctuations and longer seasonal changes.



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