Although height is normally relative to a plane of reference, most measurements of height in the physical world are based upon a zero surface, known as
sea level. Both altitude and elevation, two synonyms for height, are usually defined as the position of a point above the mean sea level. One can extend the sea-level surface under the continents: naively, one can imagine a lot of narrow canals through the continents. In practice, the sea level under a continent has to be computed from gravity measurements, and slightly different computational methods exist; see
Geodesy, heights. In addition to vertical position, the vertical extent of geographic landmarks can be defined in terms of
topographic prominence. For example, the highest mountain (by elevation in reference to sea level) belongs to
Mount Everest, located on the border of
Nepal and
Tibet, China; however the
tallest mountain, by measurement of apex to base, is
Mauna Kea in
Hawaii, United States.
In geodesy Geodesists formalize mean sea level (MSL) by means of the
geoid, the equipotential surface that best fits MSL. Then various types of height (normal, dynamic, orthometric, etc.) can be defined, based on the assumption of density of topographic masses necessary in the continuation of MSL under the continents. A purely geometric quantity is the
ellipsoidal height, reckoned from the surface of a
reference ellipsoid, see
Geodetic system, vertical datum. ==In aviation==