The shape of our earth is not perfectly spherical. So when we try to approximate the shape of it, we have to find a appropriate model. We've seen earlier on that such a model can be an ellipsoid. The **geoid** is a more advanced reference surface which is used to approximate the shape of the Earth and to measure elevations (see orthometric elevation).

Any point on the **geoid **is subject to the same level of gravity and the earth's geoid is set at the mean sea level.

To compare the difference between geoid and ellipsoid. The deviation between the Geoid and a reference ellipsoid is called geoid separation (N).See figure below.