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ISO 19139 Metadata Implementation Specification
FALSE
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DGS_WT_NORM
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Projected
GCS_WGS_1984
Linear Unit: Meter (1.000000)
WGS_1984_Web_Mercator_Auxiliary_Sphere
<ProjectedCoordinateSystem xsi:type='typens:ProjectedCoordinateSystem' xmlns:xsi='http://www.w3.org/2001/XMLSchema-instance' xmlns:xs='http://www.w3.org/2001/XMLSchema' xmlns:typens='http://www.esri.com/schemas/ArcGIS/10.6'><WKT>PROJCS["WGS_1984_Web_Mercator_Auxiliary_Sphere",GEOGCS["GCS_WGS_1984",DATUM["D_WGS_1984",SPHEROID["WGS_1984",6378137.0,298.257223563]],PRIMEM["Greenwich",0.0],UNIT["Degree",0.0174532925199433]],PROJECTION["Mercator_Auxiliary_Sphere"],PARAMETER["False_Easting",0.0],PARAMETER["False_Northing",0.0],PARAMETER["Central_Meridian",0.0],PARAMETER["Standard_Parallel_1",0.0],PARAMETER["Auxiliary_Sphere_Type",0.0],UNIT["Meter",1.0],AUTHORITY["EPSG",3857]]</WKT><XOrigin>-20037700</XOrigin><YOrigin>-30241100</YOrigin><XYScale>148923141.92838538</XYScale><ZOrigin>-100000</ZOrigin><ZScale>10000</ZScale><MOrigin>-100000</MOrigin><MScale>10000</MScale><XYTolerance>0.001</XYTolerance><ZTolerance>0.001</ZTolerance><MTolerance>0.001</MTolerance><HighPrecision>true</HighPrecision><WKID>102100</WKID><LatestWKID>3857</LatestWKID></ProjectedCoordinateSystem>
20190703
11515400
20190703
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ISO19139
Delaware Geological Survey
(302)-831-2833
302-831-3579
University of Delaware Delaware Geological Survey Building
Newark
DE
19716
M-F 8:00AM-4:00PM
ArcGIS Metadata
1.0
Delaware Geological Survey
(302)-831-2833
302-831-3579
University of Delaware Delaware Geological Survey Building
Newark
DE
19716
US
delgeosurvey@udel.edu
Raster Dataset
2005-01-01
Delaware Geological Survey
DGS DGIR Web Site
Matthew J. Martin and A. Scott Andres
DGS Digital Data Products
DP05-01, DP05-03, and DP05-04
Water-Table Elevation (normal conditions)
<DIV STYLE="text-align:Left;"><DIV><P><SPAN>This digital product contains gridded estimates of water-table (wt) elevation under normal conditions for Delaware. 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. The grids have 30-m horizontal and 1-ft vertical resolutions. In the accompanying digital data, grid world files and ground-water level observation data are in UTM-18N, 1983 projection in meters and elevations are in feet, NAVD 1988. Files are in ESRI, Inc., grid format. These data were combined from DGS Digital Data Products DP05-01, DP05-03, and DP05-04 Digital Water-Table Data for Sussex, Kent, and New Castle counties, Delaware, respectively. REFERENCES CITED Andres, A. S., and Martin, M. J., 2005, Estimation of the water-table surface for the Inland Bays watershed, Delaware: Delaware Geological Survey Report of Investigations No. 68, 20p. ESRI, 2004, ArcMap v. 9, Redlands, California. Sepulveda, N., 2003, A statistical estimator of the spatial distribution of the water-table altitude: Ground Water, vol. 41, p. 66-71.</SPAN></P></DIV></DIV>
This work is part of a larger effort to provide estimates of water-table elevations and depths to water for the Coastal Plain portion of Delaware. These maps will be used in risk assessments and for environmental management decision-making.
Matthew J. Martin and A. Scott Andres
Delaware Geological Survey
(302)-831-2833
302-831-3579
University of Delaware Delaware Geological Survey Building
Newark
DE
19716
US
delgeosurvey@udel.edu
Mon - Fri; 8:00am to 4:30pm
New Castle
Milton
South Bethany
Blades
Felton
Arden
Kent County
Kenton
Wyoming
Ardencroft
Bethel
Bethany Beach
Greenwood
Dagsboro
Seaford
Little Creek
Frankford
Millsboro
Ellendale
Millville
Hartly
Elsmere
Camden
Lewes
Farmington
Townsend
Woodside
Henlopen Acres
Wilmington
Harrington
Viola
Leipsic
Selbyville
Smyrna
Houston
Bridgeville
Rehoboth Beach
Ocean View
Newark
Middletown
Fenwick Island
Milford
Georgetown
New Castle County
Delmar
Frederica
Magnolia
Laurel
Claymont
Newport
Bellefonte
Odessa
Delaware
Clayton
Sussex County
Dover
Slaughter Beach
groundwater
Water Table
inlandWaters
Delaware Hydrology
New Castle
Milton
South Bethany
Blades
Felton
groundwater
Arden
Kent County
Kenton
Wyoming
Ardencroft
Bethel
Bethany Beach
Greenwood
Dagsboro
Seaford
Little Creek
Frankford
Millsboro
Ellendale
Millville
Hartly
Water Table
inlandWaters
Elsmere
Camden
Lewes
Farmington
Townsend
Woodside
Henlopen Acres
Wilmington
Harrington
Viola
Leipsic
Selbyville
Smyrna
Delaware Hydrology
Houston
Bridgeville
Rehoboth Beach
Ocean View
Newark
Middletown
Fenwick Island
Milford
Georgetown
New Castle County
Delmar
Frederica
Magnolia
Laurel
Claymont
Newport
Bellefonte
Odessa
Delaware
Clayton
Sussex County
Dover
Slaughter Beach
The Delaware Geological Survey (DGS) is constantly gathering data from multiple sources, interpreting data, and reflecting its interpretations in a variety of data formats. DGS's interpretations are conceptualized in these grids of Water-Table Elevation for Sussex County, DE. The water table is a continuous surface; however, observations of the surface exist at irregularly spaced locations. In this instance, regularly spaced grids of water-table elevations were estimated from site-specific observational data and are the model used to represent the water-table surface. Reasonable efforts have been made by the DGS to verify that the digital data provided hereon accurately interpret the source data used in its preparation. These are estimated surfaces and they may be inappropriate for some applications. Detailed site-specific investigation may be required for evaluating individual sites. Persons wishing to apply the data in these grids to more detailed scales are encouraged to contact the DGS office for advisement. Nothing contained nerein shall be deemed an expressed or implied waiver of the sovereign immunity of the State of Delaware or its duly authorized representatives, agents, or employees.
<DIV STYLE="text-align:Left;"><DIV><P><SPAN>The Delaware Geological Survey (DGS) is constantly gathering data from multiple sources, interpreting data, and reflecting its interpretations in a variety of data formats. DGS's interpretations are conceptualized in these grids of Depth to Water for Delaware. The water table is a continuous surface; however, observations of the surface exist at irregularly spaced locations. In this instance, regularly spaced grids of water-table elevations were estimated from site-specific observational data and are the model used to represent the water-table surface. Reasonable efforts have been made by the DGS to verify that the digital data provided herein accurately interpret the source data used in its preparation. These are estimated surfaces and they may be inappropriate for some applications. Detailed site-specific investigation may be required for evaluating individual sites. Persons wishing to apply the data in these grids to more detailed scales are encouraged to contact the DGS office for advisement. Nothing contained herein shall be deemed an expressed or implied waiver of the sovereign immunity of the University of Delaware and the State of Delaware or their duly authorized representatives, agents, or employees. Additional Information In order to provide complete data coverage for the entire Coastal Plain, Sussex County, Kent County, and New Castle County grids (Digital Products DP05-01, DP05-03, and Dp05-04) were merged together. Further manipulation of these data grids by the user is done solely at the descretion of the user.</SPAN></P></DIV></DIV>
ground condition
2005-01-01
Version 6.2 (Build 9200) ; Esri ArcGIS 10.6.1.9270
1
-75.789023
-75.048721
39.839532
38.451186
30-meter resolution based on the grid cell.
The raster grid cell has a 1-foot vertical resolution.
+/- 0.5 foot
VAT_WT_NORM1
179
Table
ObjectID
Internal feature number.
ESRI
Sequential unique whole numbers that are automatically generated.
0
OBJECTID
OID
0
4
Value
0
Value
Integer
0
4
Water-table elevation in feet relative to North American Vertical Datum of 1988.
Count
0
Count
Double
0
8
This refers to the total number of grid cells within the raster grid that have a particular "value" (see above).
dataset
EPSG
8.8(9.3.1.2)
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6643
2747
30.000000
30.000000
8
1
Upper Left
FALSE
LZ77
1
pixel codes
SDR
FALSE
row and column
30.000000
30.000000
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