GM15 Geologic Map of the Georgetown Quadrangle, Delaware
The geologic history of the surficial geologic units of the Georgetown Quadrangle is primarily that of deposition of the Beaverdam Formation and its subsequent modification by erosion and deposition of younger stratigraphic units. The age of the Beaverdam Formation is uncertain due to the lack of age-definitive fossils within the unit. Stratigraphic relationships in Delaware indicate that it is no older than late Miocene and no younger than early Pleistocene. Regional correlations based on similarities of depositional style, stratigraphic position, and sediment textures suggest that it is likely late Pliocene in age; correlative with the Bacons Castle Formation of Virginia (Ramsey, 1992, 2010).
- Beaverdam Formation
- Carolina Bay deposits
- Cat Hill Formation
- cross-sections
- dune deposits
- geology
- Georgetown
- Harbeson
- mapping
- Miocene
- Neogene
- Pliocene
- St. Marys Formation
- STATEMAP
- surficial geology
- Sussex County
- swamp deposits
- topography
- Turtle Branch Formation
- upper Pleistocene
- upper Pliocene
- wetlands
- lower Pliocene
- middle Pleistocene
- Miocene
- Pleistocene
- Tertiary Period
- upper Miocene
- lower Pleistocene
- middle Miocene
- lower Miocene
Stream Station: Millsboro Pond Outlet at Millsboro
USGS 01484525 MILLSBORO POND OUTLET AT MILLSBORO, DE
Water Conditions Summary Groundwater Graphs
Water Conditions Summary Groundwater Well Hydrographs
Water Conditions Summary Precipitation Graphs
Water Conditions Summary Precipitation Graphs
Water Conditions Summary Station Map
Map displaying all observing stations monitored by DGS for current and long-term conditions as part of the Water Conditions Summary for Delaware.
Groundwater Station: DGS Well Nc13-03
DGS Well Nc13-03
Meteorological Station: Greenwood
Greenwood Meterological Station
Meteorological Station: City of Lewes
City of Lewes Meteorological Station
Hydrologic Stratigraphic Chart
- aquifer
- Cheswold aquifer
- Columbia aquifer
- Cretaceous Period
- groundwater recharge
- Holocene
- hydrogeology
- Kent County
- Magothy aquifer
- Manokin aquifer
- Milford aquifer
- Miocene
- Mount Laurel aquifer
- Neogene
- New Castle County
- Oligocene
- Piney Point aquifer
- Pliocene
- Pocomoke aquifer
- Rancocas aquifer
- stratigraphy
- Sussex County
- unconfined aquifer
- Upper Cretaceous
- upper Eocene
- upper Holocene
- upper Pleistocene
- upper Pliocene
- Eocene
- Jurassic Period
- Lower Cretaceous
- lower Holocene
- lower Pliocene
- middle Eocene
- middle Pleistocene
- Miocene
- Paleogene
- Pleistocene
- Tertiary Period
- upper Miocene
- lower Eocene
- lower Pleistocene
- middle Miocene
- Paleocene
- Triassic Period
- lower Miocene
- Mesozoic Era
Hydrogeologic Resources for Delaware
Hydrogeologic data and information for Delaware. This includes the Water Conditions Report, groundwater well data, links to real-time data from DEOS and USGS, and other general information about Delaware's hydrogeology.
Summary of Water Conditions in Delaware
Delaware Water Conditions Report for current and historical periods of record.
Groundwater Station: DGS Well Qe44-01
DGS Well Qe44-01
Groundwater Station: DGS Well Mc51-01a
DGS Well Mc51-01a
Meteorological Station: Town of Selbyville
Town of Selbyville Meterological Station
Meteorological Station: Georgetown Sussex County Airport
Georgetown NWS Meterological Station
Stream Station: Nanticoke River near Bridgeville
USGS 01487000 NANTICOKE RIVER NEAR BRIDGEVILLE, DE
Digital Water-Table Data for Sussex County, Delaware (Digital Data Product No. 05-01)
This digital product contains gridded estimates of water-table (wt) elevation and depth to water (dtw) under dry, normal, and wet conditions for Sussex County, Delaware. Files containing the point data used to create the grids are also included. This work is the final component of a larger effort to provide estimates of water-table elevations and depths to water for the Coastal Plain portion of Delaware. Mapping was supported by the Delaware Department of Natural Resources and Environmental Control and the Delaware Geological Survey.
These grids were produced with the same multiple linear regression (MLR) method as Andres and Martin (2005). Briefly, this method consists of: identifying dry, normal, and wet periods from long-term observation well data (Nc45-01, Ng11-01, Qe44-01); estimating a minimum water table (Sepulveda, 2002) by fitting a localized polynomial surface to elevations of surface water features (e.g., streams, swamps, and marshes); and computing a second variable in the regression from water levels observed in wells. A separate MLR equation was determined for dry, normal, and wet periods, and these equations were used in ArcMap v.9 (ESRI, 2004) to estimate grids of water-table elevations and depths to water. Grids produced in this project were merged with those previously completed for eastern Sussex and smoothed to minimize edge effects.



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