CoordCalc

How to Convert Easting and Northing to Latitude and Longitude

People expect this conversion to be a formula, the way a temperature conversion is a formula. It is not. An easting and a northing are metres on a flat projected plane, and getting back to latitude and longitude means inverting the projection that produced them — which needs the zone, the hemisphere and the datum before any arithmetic can start. This guide covers what must be present, what the calculation actually does, and the mistakes that send a point hundreds of kilometres away.

GuideUpdated 9 October 2026Inverse projection

Three things you need before you begin

  1. The zone number. The same easting and northing exists in all 60 UTM zones and in every State Plane zone. Without the zone there is no answer to compute — there are sixty answers.
  2. The hemisphere, or the band letter. Northing is measured from the equator in the north and from 10,000,000 m at 80° S in the south, so the sign convention has to be known.
  3. The datum. WGS84 and NAD83 are nearly identical in practice; NAD27 is not, and can differ by up to about 100 m. Choosing the wrong datum produces a result that is confidently wrong.

If a coordinate arrives as just two numbers, the honest answer is that it is not yet a coordinate. That is worth saying out loud, because half of all conversion failures are not arithmetic failures — they are missing-metadata failures.

What the calculation does

Every projected grid is built from a small set of defining parameters. For UTM they are: a central meridian (177° W plus 6° per zone), a scale factor of exactly 0.9996 along it, a false easting of 500,000 m, a false northing of 0 in the north or 10,000,000 m in the south, and the GRS80 or WGS84 ellipsoid. The conversion runs in four steps:

1. ΔE = easting − 500,000   (metres east of the central meridian, scaled)
2. M  = (northing − false northing) ÷ 0.9996   (meridian arc from the equator)
3. φ₁ = footpoint latitude, inverted from M by series
4. φ, λ from φ₁, ΔE and the ellipsoid's eccentricity

Step 3 is the part that has no closed form and is why the calculation is done by series expansion or iteration rather than by a single expression. The series used by practical software — and by the converters on this site — agree with the official reference implementations to well under a millimetre, so precision is never the limiting factor.

Worked example

Take the UTM reference 17T 630084 4833438. Zone 17 has a central meridian of 81° W, and the band T confirms the northern hemisphere.

StepValueMeaning
Easting − false easting630,084 − 500,000 = 130,084 mPoint lies 130 km east of 81° W
Northing ÷ 0.99964,833,438 ÷ 0.9996 ≈ 4,835,372 mMeridian arc from the equator
Invert to footpoint latitude≈ 43.633° NLatitude of the point on the central meridian
Solve for latitude and longitude43.642562° N, 79.387143° WFinal result, WGS84

Two checks are worth running on any result. First, the longitude must land inside the zone's 6° band: 79.387° W sits comfortably inside 78° W to 72° W, so the zone and the answer agree. Second, the latitude must sit inside the band: 43.64° N is inside 40° N to 48° N for band T. If either check fails, the zone number or the hemisphere is wrong — the arithmetic is not.

The swap error, and how to catch it

Writing northing first is the classic mistake, and it is easy to make because latitude and longitude are conventionally written the other way round. A swapped UTM coordinate usually produces a latitude that is wildly out of range for its band, since a northing of 4,833,438 gets read as an easting placing the point 4,333 km east of the central meridian, far outside any zone.

The practical rule: an easting in a UTM coordinate is almost always six digits and between about 100,000 and 900,000. A northing is six or seven digits. If a value over 1,000,000 appears in the easting position, or a value under 1,000,000 appears in the northing position north of the equator, the pair is probably reversed.

Do not convert in a spreadsheet with a home-made formula. Transverse Mercator inverse series have several terms and a sign convention that differs between zones in the southern hemisphere. A spreadsheet formula that is one term short will look right at the zone's central meridian and be tens of metres out at the zone edge — which is the worst kind of error, because it passes every test near the middle and fails only where the work is.

State Plane and other grids

The same four steps apply to any projected grid, including US State Plane coordinates. What changes is the parameter set. A State Plane zone is defined by either two standard parallels (Lambert Conformal Conic, for zones that run east-west) or a central meridian with its own scale factor (Transverse Mercator, for zones that run north-south), plus a false origin and a false easting and northing. And State Plane records add one more wrinkle: coordinates may be in metres, in US survey feet or in international feet, and choosing the wrong one shifts the answer by about two parts per million — harmless in a car park, significant on a section line.

Tools used in this article

Related guides

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