Datum Shift Explained: Why Your Coordinates Change
A "Datum Shift" occurs when you describe a single point on the physical earth using two different geodetic datums, resulting in two mathematically different coordinates. If this shift is ignored during mapping or construction, the physical asset will be placed in the wrong location — sometimes off by hundreds of meters.
Why Do Datums Shift?
Datums shift for two primary reasons:
- Better Math: In 1927, the US defined the NAD27 datum using triangulation stations entirely on land. In 1983, satellites provided a much more accurate center-of-mass model of Earth (NAD83/WGS84). Switching from NAD27 to NAD83 causes coordinates to shift by tens to hundreds of meters.
- Plate Tectonics: The continents move on tectonic plates. If a datum is pinned to the physical rock of North America (a "Plate-Fixed" datum like NAD83), its coordinates stay relatively constant locally over time. If a datum is pinned to the center of Earth's mass (an "Earth-Fixed" datum like WGS84), the continent literally drifts away from the coordinate grid over time by a few centimeters a year.
Real-World Consequences of Datum Shifts
Ignoring datum shifts is a leading cause of liability claims against GIS professionals, engineers, and surveyors.
→ Survey Negligence Liability
How to Manage the Shift
If your project involves data from multiple sources, you must verify the coordinate system and the datum.
- Apply a Transformation: A datum transformation is a mathematical formula (such as Helmert 7-parameter or NADCON) that converts a coordinate from datum A to datum B. It is never perfect, but it is necessary.
- Check the Epoch: For highly precise modern datums (like WGS84 or ITRF), you must also specify the "Epoch" (the specific date the measurement was valid), because tectonic drift guarantees the coordinate will change over time.
- Maintain Metadata: Never store a coordinate simply as "Lat/Long". It must be stored as "Lat/Long (NAD83 2011 Epoch 2010.0)" or similar.
Test a datum shift locally using our coordinate conversion tool, switching between WGS84 and local grids (like NAD27 or Tokyo Datum):
→ Coordinate and Datum ConverterFAQ
How large is the shift between NAD27 and NAD83?
In the continental United States, it is generally between 10 meters and 100 meters, depending on your location. The shift is not uniform across the country.
Is WGS84 drifting relative to NAD83?
Yes. Because WGS84 is tied to the center of the Earth and the North American continent is slowly moving, the physical difference between the two systems grows by roughly 1 to 2.5 centimeters every year.
Does a map projection cause a datum shift?
No. A map projection (like UTM or Web Mercator) flattens the datum onto 2D paper. The datum is the 3D globe underneath the projection. You can have UTM coordinates in WGS84 and UTM coordinates in NAD27. They will not line up.
See also: WGS84 vs NAD83 | EPSG:4326 vs 3857 | Reference Standards
US State Plane (SPCS) Converters & Local Guides
Professional engineering and surveying transformations from state-specific conformal grids to GPS WGS84.
Using the wrong datum or applying coordinates without grid-to-ground correction can cause 1–400 metre positional errors — a leading cause of surveying negligence claims and contract disputes.