Distance to Poles
Measure great-circle distance from your location to the geographic poles.
By Aryan Khan, Founder & Editor · Updated October 2026
For example, New York sits approx. 3,405 miles (5,481 km) from the North Pole and approx. 9,031 miles (14,535 km) from the South Pole — polar distance is just latitude, measured.
How to use Distance to Poles
Two fixed points, every place on Earth, one clean piece of geometry:
Distance to Poles measures the great-circle distance from any place to the North Pole and South Pole. Because the poles sit at the ends of the Earth's axis, the answer is latitude geometry: your distance to the nearer pole depends only on how far your latitude is from ninety degrees.
- 1Set your place and a pole coordinate.
- 2Read great-circle distance.
What people use Distance to Poles for
1. Geography teaching
The poles make latitude tangible: a class can watch the North Pole distance shrink by about 69 miles for every degree travelled north, because that is literally what a degree of latitude is.
2. Expedition and aurora context
Polar-night and aurora questions are latitude questions. This measure frames how 'polar' a place like Tromsø or Fairbanks really is before the detailed planning starts.
3. Trivia with receipts
Which is closer to a pole, Reykjavík or Anchorage? The argument ends here, with a method anyone can rerun — the Distance Between Two Places tool then settles the city-to-city version.
4. Antipode and extremes exploration
Pair this with the antipode tools to explore the planet's extremes: farthest from the pole, farthest from your own antipode, closest to the axis ends.
Worked examples
New York (40.7128° N): to the North Pole approx. 5,480.5 km (3,405.4 mi) — that is (90 − 40.7128) = 49.2872° of arc; to the South Pole approx. 14,534.6 km (9,031.4 mi). The two always sum to the half-circumference, approx. 20,015 km.
London (51.5072° N) to the South Pole: approx. 15,734.9 km (9,777.2 mi) — near the maximum any northern city can be from the far pole. Its North Pole distance is correspondingly shorter, which the tool shows side by side.
The latitude ladder
Distance to the North Pole depends only on latitude: it is (90° − latitude) of arc on the site model. Read your latitude, read your polar distance.
| Latitude | To North Pole (km) | To North Pole (mi) | To South Pole (km) |
|---|---|---|---|
| 80° N | 1,112.0 | 690.9 | 18,903.2 |
| 60° N | 3,335.9 | 2,072.8 | 16,679.3 |
| 51.5° N (London) | 4,280.6 | 2,659.8 | 15,734.9 |
| 40.7° N (New York) | 5,480.5 | 3,405.4 | 14,534.6 |
| 30° N | 6,671.7 | 4,145.5 | 13,343.4 |
| 0° (Equator) | 10,007.6 | 6,218.4 | 10,007.6 |
| 30° S | 13,343.4 | 8,291.1 | 6,671.7 |
| 60° S | 16,679.3 | 10,363.7 | 3,335.9 |
Figures are (90 ∓ latitude) × 111.195 km per degree on the mean sphere, rounded — the tool computes the exact haversine for your point.
How to interpret the result
The most common errors come from using a correct result to answer the wrong geographic question. Keep these points in mind for Distance to Poles:
- Always confirm which distance you need before quoting one: straight-line for physical questions, road distance for driving, and network time for schedules. The three can differ by half again in mountainous or island geography, and quoting the wrong one is the most common distance mistake in reports.
- Remember that bearings are true-north by default. If you are transferring a bearing to a magnetic compass, add (or subtract) your local declination — it exceeds 10° in many inhabited regions and flips hemispheres of behaviour.
Limits & appropriate use
The honest limits here are about category, not quality: great-circle math is near-exact, but it answers 'how far over the surface', not 'how far as driven, flown or walked'. Airline distances follow airways and winds; odometers follow detours; hikers follow switchbacks. Quoting a straight-line number into a fuel budget is the classic misuse, which is why the tools keep the ladder visible — crow-flies, road, time — and label each rung. A second limit is definitional: 'city to city' means mapped centre to mapped centre, and a suburb-to-airport question is a different measurement wearing the same sentence.
Within those bounds the numbers are durable: reproducible from coordinates alone, stable across tools that use the same radius convention, and accurate to a fraction of a percent of geodetic truth. The escalation path is short and rarely needed — ellipsoidal libraries (Karney's algorithms) for survey-grade millimetres, the routing engine for network truth, and the airline's schedule for invoice truth. Knowing which authority owns which number is the entire craft of distance literacy.
- Survey-grade millimetres → ellipsoidal geodesic libraries, not sphere math.
- Fuel and schedule planning → road routing plus your congestion buffer.
- Airline invoicing → carrier distance tables (airways ≠ great circles).
Data & methodology
The shared distance workspace measures two selected points; it does not automatically select or compare the poles.
For source details, licences and model limitations, see Data Sources and Methodology.
Key terms worth knowing
- Great circle
- A circle centred on Earth's centre; its arcs are the shortest surface paths.
- Haversine
- The standard stable formula for great-circle distance on a sphere.
Editorial guidance: MapBench explains the method and limitations so the tool can be used as a transparent reference, not as a black-box answer. For legal boundaries, safety-critical routing, surveying, engineering, regulated decisions or official statistics, verify the result with the responsible authority or a qualified professional.
Category: Distance & Bearing. Results are intended for everyday analysis and planning unless a page explicitly states otherwise.
Method, assumptions & limits
- This tool’s method
- The shared distance workspace measures two selected points; it does not automatically select or compare the poles.
- Before relying on the answer
- Keep the endpoints and measurement mode fixed when comparing results. A surface separation, a compass bearing and a road distance are different outputs.
- What the result cannot establish
- A rounded coordinate or a city-centre search changes the endpoints. Do not interpret displayed decimal places as survey accuracy.
Coverage: Worldwide. Search, basemap and external data requests may use third-party services; browser-based does not mean every operation is offline. Read the source and licence notes, calculation methodology and privacy policy. If a result looks inconsistent, report a correction with the inputs and mode used.
Frequently asked questions
Clear answers about the calculation, accuracy and appropriate use.
Pole coordinates?
Geographic North Pole ≈ 90°N, 0°; South Pole ≈ 90°S.
How accurate is this distance?
The geometric calculation is suitable for planning and comparison, but the answer is only as accurate as the coordinates you provide. Road, terrain and legal distances can differ.
Can I use coordinates instead of place names?
Yes. Where the tool accepts locations, you can paste latitude and longitude directly for a more explicit input.
Why can this differ from Google Maps or a road route?
Straight-line and geodesic tools measure geometry on Earth, while road-routing tools follow an actual transport network. They answer different questions.
Why does only latitude matter?
The poles are the axis endpoints: every meridian runs into them. Moving east or west changes your longitude but not your angular distance to the pole, so the great-circle distance to a pole is set by latitude alone.
What are the poles' coordinates?
The geographic North Pole is 90° N (longitude is undefined there — every direction from it is south) and the South Pole is 90° S, where every direction is north. The tool uses those fixed points.
Is the reverse bearing from the pole meaningful?
No — and the tool will not pretend otherwise. From the North Pole every heading is 180° (south). Bearings to the pole are clean; bearings from it are a special case the geometry honestly refuses.
Geographic pole or magnetic pole?
Geographic — the axis endpoints. The magnetic poles wander (the north magnetic pole is in the Canadian Arctic) and belong to the Magnetic Declination tool's subject, not this one.
Why do the two distances sum to about 20,015 km?
Because pole-to-pole along any meridian is a half circumference: π × 6,371.0088 km ≈ 20,015 km. Your two distances are the two pieces of that arc through your meridian.
Can a place be equidistant from both poles?
Yes — everywhere on the equator, at approx. 10,007.6 km (6,218.4 mi) from each. It is the only parallel with that property.
Does the tool work in the southern hemisphere?
Yes — the ladder simply reads the other way: southern places are close to the South Pole and far from the North.
Related tools and resources
For the opposite extreme — the point furthest from you in every direction — the Antipode Finder is the companion tool; the general measure is Distance Between Two Places; and the latitude arithmetic behind this page is explored in Latitude Degrees to Nautical Miles.
More free tools
Sources, methodology & editorial trust
- ✓ Browser-first processing where supported
- ✓ External sources are documented
- ✓ No account required for public tools
- ✓ Review data sources
Calculations are documented with their assumptions, limitations and source context rather than presented as unexplained answers.
Reviewed and maintained by Aryan Khan, Founder & Editor of MapBench.
Part of our distance calculators hub
Distance to Poles sits in the distance calculators cluster, alongside 28 other tools that answer neighbouring questions with different methods or datasets.
You may also need
When this answer is only part of the job, these clusters cover the next step.
Read the guide behind this tool
Distance Calculation: Haversine, Geodesics & When It Matters — Why flat map arithmetic fails over large distances, what the haversine formula does, and when a full ellipsoidal geodesic is the better choice.