geoid (Geography Dictionary)

geoid : The shape that the surface of the Earth’s oceans would take under the influence of Earth’s gravity and rotational acceleration alone, in the absence of other influences such as winds and tides. It is often characterized as the precise mathematical figure of the Earth: a smooth but irregular gravitational equipotential surface at every point of which, by definition, the direction of the force of gravity is always perpendicular and spirit levels are always parallel. Its shape results from anomalies in the Earth’s gravitational field caused by the uneven distribution of mass within and on the Earth’s surface. A reference ellipsoid is an idealized approximation of the more complex and accurate geoid.