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Encyclopedia > Geodetic datum

A Geodetic Datum is an adjustment to position of origin and shape of the planet, used by cartographers and satellite navigation systems to translate positions indicated on their products to their real position on earth.


Examples of common Geodetic Datums are:

The difference between WGS84 and OSGB36 is 140 metres / 450 feet, which for most navigational purposes is an insignificant error. For other applications, such as surveying and dive site location for SCUBA divers, 140 metres is an unacceptably large error.


  Results from FactBites:
 
World Geodetic System - Wikipedia, the free encyclopedia (1839 words)
As a result, the elevations in the datums are referenced to the geoid, a surface that is not readily found using satellite geodesy.
(The datums are relatively oriented with respect to different portions of the geoid by the astro-geodetic methods already described.) The sole contribution of satellite data to the development of WGS 60 was a value for the ellipsoid flattening which was obtained from the nodal motion of a satellite.
In January 1966, a World Geodetic System Committee composed of representatives from the Army, Navy and Air Force, was charged with the responsibility of developing an improved WGS needed to satisfy mapping, charting and geodetic requirements.
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