Gravity, Magnetic, and Seismic Geophysical Methods
Classified in Physics
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Gravity Method
The weight of any body depends on the force of gravity at that location.
The force of gravity varies with elevation, rock density, latitude, and topography.
When a mass is suspended from a spring, the amount of spring stretching is proportional to the force of gravity.
F=m.g
Where:
- g: Acceleration of gravity.
Since mass is constant, then stretch variations determine the variations in the acceleration of gravity (g).
A gravimeter is an instrument used to measure (g) at stations. The readings are corrected for elevation, latitude, and topography. The normal value of (g) is subtracted from the corrected readings to compute the residual gravity.
The values of residual gravity are plotted at the measuring stations to produce a contour map... Continue reading "Gravity, Magnetic, and Seismic Geophysical Methods" »