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Summary Of: Geodetic system

Encyclodia Page On: Geodetic system

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geodesy | navigation | surveying | cartographers | satellite navigation systems | earth | earth | sphere | World Geodetic System | OSGB36 | Ordnance Survey | Great Britain | ED50 | North Pole | South Pole | Equator | True North | reference ellipsoids | surveying | SCUBA | GPS | surveying | geodesy | earth's | latitude | longitude | WGS84 | sea levels | geoid | sea level | tides | average | nautical charts | chart datum | geoid | Quebec | Canada | The same position on a spheroid has a different angle for latitude depending on whether the angle is measured from the normal (angle α) or around the center (angle β). Note that the "flatness" of the spheroid in the image is greater than that of the Earth; therefore, the corresponding difference between the "geocentric" and "geodetic" latitudes is also greater. | | normal | Local tangent plane | | Earth-centred Earth-fixed | MATLAB | World Geodetic System | Ordnance Datum | Categories | Cartography | Navigation | Geodesy | Surveying | GPS |
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Geodetic system".