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Kucks, Robert P. , 1999, Bouguer gravity anomaly data grid for the conterminous US:.This is part of the following larger work.
U.S. Geological Survey, 1993, National geophysical data grids; gamma-ray, gravity, magnetic and topographic data for the conterminous United States: U.S. Geological Survey Digital Data Series DDS-9.
This is a Raster data set. It contains the following raster data types:
The map projection used is Albers Conical Equal Area.
Planar coordinates are encoded using row and column
Abscissae (x-coordinates) are specified to the nearest 4.0
Ordinates (y-coordinates) are specified to the nearest 4.0
Planar coordinates are specified in kilometer
The horizontal datum used is Noth American Datum of 1927.
The ellipsoid used is CLARKE1866.
The semi-major axis of the ellipsoid used is 6378.20640.
The flattening of the ellipsoid used is 1/0.99661.
| Value | Definition |
|---|---|
| -0.3402823E+39 | areas for which no data are available in the grid |
| Range of values | |
|---|---|
| Minimum: | -340 |
| Maximum: | 95 |
| Units: | milligal |
| Resolution: | 0.1 |
The compilation of onshore data consisted of nearly one million Bouguer gravity anomaly values computed by using a reduction density of 2.67 grams per cubic centimeter. The offshore data consisted of approximately 800,000 free-air gravity anomaly values.USGS employees: Godson and Scheibe
(303) 236-1405 (voice)
rkucks@usgs.gov
Gravity anomalies are produced by density variations within the rocks of the Earth's crust and upper mantle. Mapping of these density variations is the primary use of gravity anomalies.
Person who carried out this activity:
(303)236-1405 (voice)
rkucks@usgs.gov
Gravity measurements made on the surface of the Earth must be corrected in various way before they can be made into an anomaly map. The free-air correction reduces the measurement to sea level by assuming there is no intervening mass as a uniform slab of constant density, and the complete Bouguer correction includes the effects of constant density topography within 166.7 km of the measurement location. A gravity reference field is subtracted from the corrected measurements to produce the free-air, simple Bouguer, or complete Bouguer anomaly. The data set constitutes many years of individual collection of gravity stations and therefore is difficult to access the precise accuracy.
Earlier collection of stations was by surveying methods. Positions were also acquired from locations on topographic maps. Recently the station latitudes, longitudes and elevations were acquired by Geopositioning Satellite (GPS) systems.
There will always be upgrades and additions to the data set that generated the grid due to regional interests.
The accuracy of the data set that generated the grid is totally dependant on the individual who collected each gravity station. In the case of a national set they would number in the hundreds. Variations would include latitude, longitude, elevation, raw gravity reading and base station control.
Are there legal restrictions on access or use of the data?
- Access_Constraints: None
- Use_Constraints: None
(303)236-1405 (voice)
rkucks@usgs.gov
USGS Digital Data Series DDS-9
The USGS has made every effort to verify the veracity of this information, but is not liable for any inaccuracies.
| Data format: | Gridded gravity anomaly data in format ArcInfo export (version 7.x) Arc-Info grid format Size: 3.5 megabytes |
|---|---|
| Network links: |
<ftp://ftpext.usgs.gov/pub/cr/co/denver/musette/pub/GEOPHYSICAL_DATA/cdrom_DDS-9/GRIDS/ARC_INFO/bouguer_sdd.e00.gz> |
(303)236-1405 (voice)
rkucks@usgs.gov