Antipode Calculator

Enter a latitude and longitude to find the exact point on the opposite side of the globe, plus how far it is across the surface or straight through the Earth.

Quick Facts

Formula
Negate latitude; shift longitude 180°
Antipode lat = −lat. Antipode lon = lon + 180° (or lon − 180° if lon > 0°), normalized to −180°...180°.
Distance
The same for every location on Earth
≈20,015 km (12,437 mi) across the surface; ≈12,742 km (7,918 mi) straight through the center, using a mean Earth radius of 6,371 km.
Ocean coverage
~71% of Earth's surface is ocean
Most land-based points have an antipode somewhere in open water.

Your Results

Calculated
Antipode latitude
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Opposite point's N/S coordinate
Antipode longitude
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Opposite point's E/W coordinate
Surface distance
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Great-circle path along Earth's surface
Through-Earth distance
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Straight line through the planet's center

Ready

Enter a latitude and longitude, then press Calculate to find the antipodal point.

How the Antipode Calculator Works

Every point on Earth has exactly one antipode: the point diametrically opposite it, as if you drilled a straight line through the planet's center and kept going until you popped out the other side. This calculator finds that point from any latitude and longitude, along with how far apart the two points are.

The formula

Given a latitude lat and longitude lon in decimal degrees:

  • Antipode latitude = −lat (flip the hemisphere — north becomes south, south becomes north, the same number of degrees from the equator).
  • Antipode longitude = lon + 180° if lon ≤ 0°, or lon − 180° if lon > 0° (shift halfway around the globe, then normalize back into the −180° to 180° range).

Because the antipode always sits at the opposite end of a line through the planet's center, the distance between any point and its antipode is fixed by Earth's size alone — it never depends on where the point is. Using a mean Earth radius of 6,371 km, two distances follow directly:

  • Surface (great-circle) distance = π × R ≈ 20,015 km (12,437 mi) — the shortest path along the globe's curved surface, exactly half of Earth's circumference.
  • Through-Earth distance = 2 × R ≈ 12,742 km (7,918 mi) — the straight-line "dig a hole" distance, equal to Earth's diameter.

Worked example

New York City sits at about 40.7128° N, 74.0060° W. Flipping the latitude gives 40.7128° S; shifting the longitude by 180° gives 105.9940° E. That antipodal point falls in the Indian Ocean, southwest of Australia — a reminder that most land-based antipodes end up in open water, since oceans cover roughly 71% of Earth's surface.

Reading the result

The two coordinate results show where the antipode is; the two distance results are constants that apply to every calculation, since any point and its antipode are always separated by the same share of Earth's circumference and diameter. To use the antipode for mapping or navigation, plug the resulting latitude and longitude directly into a map search.

Frequently Asked Questions

What is an antipode?
An antipode is the point on Earth's surface that is diametrically opposite another point - the spot you would reach by drilling a straight line through the planet's center and continuing out the other side. Every location has exactly one antipode.
How is the antipode's latitude and longitude calculated?
Negate the latitude, so a point at 40 degrees N has an antipode at 40 degrees S. Shift the longitude by 180 degrees and wrap it back into the -180 to 180 range, so a longitude of -74 degrees becomes 106 degrees (-74 + 180).
Why is the distance to the antipode always the same?
Any point and its antipode sit at opposite ends of a diameter through Earth's center, so the straight-line distance always equals Earth's diameter (about 12,742 km or 7,918 mi), and the shortest surface path always equals half of Earth's circumference (about 20,015 km or 12,437 mi), regardless of where the starting point is.
Is my antipode likely to be on land or in the ocean?
Ocean covers roughly 71% of Earth's surface, so most land locations have an antipode somewhere in the sea. A few regions are exceptions - for example, parts of South America and Southeast Asia are near-antipodal to each other.