How does acceleration due to gravity change with the shape of earth?
The variation of g over the surface of the globe is important because it provides information on variations in the shape and internal structure of the Earth.
If we rearrange F = GmMR2 substituting for M via ρ = MassVolume = M43πR3 = 3M4πR3 , we obtain:
g = 4πρRG3
If the Earth were a perfect sphere of uniform density, g would be constant over its entire surface. But if the Earth deviates from spherical (i.e. if R varies) or if there is a local density anomaly, g will vary.