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GPS Midpoint Calculator

Find the geographic midpoint between two GPS coordinates — the point exactly halfway along the great-circle path, not simply the average of the two coordinates.

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Midpoint Latitude

50.1886

Midpoint Longitude

1.1466

Spark says

Flat lay of a European map with two compasses, symbolizing travel and exploration.
Photo by Aliaksei Lepik on Pexels
Two people using a navigation app on a smartphone during a road trip
Photo by Thirdman on Pexels

Formula

φm=arctan2 ⁣(sinφ1+sinφ2, (cosφ1+Bx)2+By2)\varphi_m = \arctan2\!\left(\sin\varphi_1+\sin\varphi_2,\ \sqrt{(\cos\varphi_1+B_x)^2+B_y^2}\right)
B_x, B_y
— Intermediate great-circle midpoint terms

What is the GPS Midpoint Calculator?

This finds the point exactly halfway along the great-circle path between two coordinates — useful for planning a meeting point that's genuinely equidistant, not just the average of the two latitude/longitude numbers (which isn't the same thing on a sphere).

Use this when picking a fair meeting point between two people traveling from different locations, finding a central point for planning purposes between two distant offices or cities, or understanding why simply averaging two coordinates doesn't give a true midpoint.

How to use it

  1. 1 Enter the first location's latitude and longitude.
  2. 2 Enter the second location's latitude and longitude.

Understanding GPS Midpoint Calculator

Finding the midpoint between two coordinates seems like it should reduce to simple averaging — add the two latitudes and divide by two, do the same for longitude — and for points that are reasonably close together, that approximation works well enough that the distinction rarely matters in practice. Over longer distances, though, simple averaging diverges from the true geographic midpoint in a way that becomes increasingly significant, and understanding why requires thinking about the problem in three dimensions rather than two.

Latitude and longitude describe a position on a sphere, but simple arithmetic averaging treats them as if they were flat, independent coordinates on a grid — which is a reasonable approximation locally (over short distances, the Earth's surface is close enough to flat that the distortion is negligible) but breaks down over longer distances precisely because the sphere's curvature becomes significant. The proper way to find a true midpoint is to convert both points into three-dimensional Cartesian coordinates (thinking of each point as sitting on the surface of a sphere in 3D space), find the actual midpoint of the straight line connecting those two 3D points, then project that midpoint back onto the sphere's surface — which is mathematically equivalent to finding the point exactly halfway along the great-circle arc connecting the two original points. This is the calculation this tool performs, even though the formula itself is expressed directly in terms of latitude and longitude rather than requiring an explicit 3D conversion step.

The practical gap between simple coordinate averaging and the true great-circle midpoint grows with distance between the two original points and can also be affected by how far apart their longitudes are, since longitude lines converge toward the poles. For two points a few kilometers apart within the same city, the difference between the two methods is negligible. For two points thousands of kilometers apart — say, one city on each coast of a continent — the difference becomes clearly noticeable, potentially placing a simply-averaged 'midpoint' meaningfully off from the true geographic midpoint.

It's worth being clear about what a geographic midpoint is and isn't useful for. It answers a purely geometric question — what point sits exactly halfway along the shortest path between two locations — which is a genuinely different question from 'what's the fairest meeting point in terms of travel time or convenience.' Two people traveling from different cities toward a calculated midpoint might face very different actual travel times, depending on available roads, flights, or terrain between each starting point and the midpoint — the geographic calculation is a solid, unbiased starting point for that conversation, but real-world travel logistics often warrant adjusting the actual chosen meeting point away from the pure geographic midpoint.

Worked examples

Advantages

  • Calculates the true great-circle midpoint, not the mathematically different (and for long distances, noticeably wrong) simple average of latitude and longitude.
  • Works for any two points on Earth, including ones on opposite sides of the globe.
  • Useful alongside the distance and bearing calculators for full route or meeting-point planning.
  • Gives an exact geographic point that can be looked up on any mapping tool.

Limitations

  • This is the geographic (great-circle) midpoint, not necessarily a convenient meeting point — travel time to that midpoint can differ significantly for each person depending on roads and transport options.
  • The calculated midpoint may fall somewhere impractical (open ocean, a mountain, restricted land) — it's a pure geographic calculation, not a suggestion informed by what's actually located there.

Common mistakes

  • ⚠️ Averaging two coordinates' latitude and longitude directly instead of using the proper great-circle midpoint formula — for points that are close together this is a reasonable approximation, but for more distant points it produces a noticeably wrong result.
  • ⚠️ Assuming the geographic midpoint is also the fairest meeting point in terms of travel time — road networks, flight availability, and terrain mean travel time to the midpoint is rarely identical for both parties.
  • ⚠️ Not checking what's actually located at the calculated midpoint before treating it as a genuine destination — it might land in the middle of a lake, forest, or otherwise impractical location.

Tips

  • 💡 After calculating the geographic midpoint, look it up on a map to confirm it's a practical location, or search for the nearest town or landmark to that point.
  • 💡 For a genuinely fair meeting point in terms of travel time (not just distance), consider each person's actual transport options, not just raw geographic distance to the midpoint.
  • 💡 Pair this with the distance calculator to see how far each person would need to travel to reach the midpoint.
  • 💡 For very close points (within a city, for instance), simple coordinate averaging and the true great-circle midpoint will be nearly identical — the distinction matters most over longer distances.

Real-life uses

  • Picking a fair meeting point between friends or colleagues traveling from different cities
  • Finding a central point for planning purposes between two offices, branches, or facilities
  • Estimating a rendezvous point for a hiking, sailing, or aviation route
  • Understanding the true geographic center between any two locations for general reference

Frequently asked questions

Is the midpoint just the average of the two latitudes and longitudes?

No — because the Earth is a sphere, simply averaging coordinates gives a slightly different (and for longer distances, noticeably different) point than the true great-circle midpoint.

Why does the gap between simple averaging and the true midpoint grow with distance?

Simple averaging treats latitude and longitude as if they were flat coordinates, which is a reasonable local approximation but ignores the sphere's curvature — that ignored curvature becomes more significant as the distance between points increases.

Is the geographic midpoint always the fairest meeting point?

Not necessarily in terms of travel time — road networks, flight availability, and terrain mean two people can face very different actual travel times to reach the same geographic midpoint.

What if the calculated midpoint falls somewhere impractical, like the ocean?

That can happen, since this is a pure geometric calculation with no awareness of what's actually located at that point — check the result on a map and consider looking for a practical location near the calculated midpoint instead.

Sources & references