|This article does not cite any references or sources. (May 2014)|
A geographical pole, also known as a geographic pole, is either of the two points on a planet, moon or other relatively large rotating body where the body's axis of rotation meets its surface. As with Earth's North and South Poles, they are usually called that body's "north pole" and "south pole", one lying 90 degrees in one direction from the body's equator and the other lying 90 degrees in the opposite direction from the equator.
Perturbations in a body's rotation mean that geographical poles are prone to "wander" slightly on its surface. Every few years, for instance, the Earth's North and South Poles vary cyclically by a few metres (This phenomenon is distinct from axial precession, which, in Earth's case, means the angle of both its axis and surface, moving together, varies very slowly over tens of thousands of years.). As cartography requires exact and unchanging coordinates, the averaged locations of geographical poles are taken as fixed cartographical poles (cartographic poles) and become the points where the body's great circles of longitude intersect.