Geophysical ground measurements, gravity interpolated (overall)

Measurements of gravity can be used to map variations in mass distribution in the Earth's crust. These variations are due to differences in the composition of the bedrock. Geophysical ground measurements, gravity interpolated (overall) contains grid data that illustrates the variations found in Sweden's gravity field, expressed as Bougueranomaly. From point-by-point measurements of gravity throughout Sweden, Bougueranomalier (mGal) has been calculated in the reference field RG82. These have since been gridded with the cell size 500m x 500m. From the grid, co-ordinate Bougueranomalies have been extracted with the same point spacing corresponding to the grid cell size to a csv file.