Find the antipodal point (opposite side of Earth) for any coordinates. Visualize the exact location diametrically opposite to your position on the globe.
Ever wondered what's on the exact opposite side of the Earth from where you stand? The antipodal point — or antipode — is the location diametrically opposite any point on Earth's surface. If you could drill a straight line through the center of the planet, you'd emerge at your antipode. This calculator instantly computes that point for any set of geographic coordinates.
Contrary to popular belief, most land-based antipodes don't correspond to other land masses. In fact, only about 4% of Earth's land surface has a land antipode. If you're in North America, your antipode is almost certainly in the Indian Ocean. Europeans find their antipodes near New Zealand and in the Pacific. This calculator shows you exactly where your opposite point falls and provides details about the nearest landmass.
Our Antipode Calculator is useful for geography education, travel planning curiosity, satellite communication analysis, and understanding Earth's geometry. Enter any latitude and longitude — or choose from popular city presets — and instantly discover what lies on the other side of the world. The tool also calculates the great-circle distance through Earth's center and shows the time zone difference.
Satisfy geographic curiosity, teach Earth geometry concepts, or plan around-the-world routes. This calculator instantly shows the opposite side of the globe for any location. This tool is designed for quick, accurate results without manual computation. Whether you are a student working through coursework, a professional verifying a result, or an educator preparing examples, accurate answers are always just a few keystrokes away.
Antipodal Latitude = -latitude Antipodal Longitude = longitude + 180° (if ≤ 0°) or longitude - 180° (if > 0°) Distance through Earth = 2 × Earth's radius ≈ 12,742 km Great Circle Surface Distance = π × Earth's radius ≈ 20,015 km
Result: -40.7128°, 105.9940°
The antipode of New York City (40.7128°N, 74.0060°W) is at 40.7128°S, 105.9940°E, which is in the Indian Ocean southwest of Australia.
The concept of antipodal points goes beyond simple geography. In mathematics, antipodal points are fundamental to topology and the study of spheres. The Borsuk-Ulam theorem states that for any continuous function from a sphere to the plane, there exists at least one pair of antipodal points that map to the same value — meaning at any given moment, there are two opposite points on Earth with exactly the same temperature and barometric pressure.
Computing an antipode is mathematically straightforward: negate the latitude and add or subtract 180° from the longitude. However, because Earth is an oblate spheroid rather than a perfect sphere, the actual "through the center" path would be slightly different from the calculated surface antipode. For practical purposes, the spherical approximation is more than sufficient.
The most notable near-antipodal city pair is Madrid, Spain and Wellington, New Zealand, which are remarkably close to being exact opposites. Parts of northern Spain are almost perfectly antipodal to New Zealand's South Island. In South America, the southern tip of Argentina is antipodal to parts of Mongolia and Russia. Hawaii's antipode falls in Botswana, Africa — one of the few cases where a US location has a land-based antipode.
Some interesting geographic antipodal facts: the entire continent of Antarctica is approximately antipodal to the Arctic Ocean. The Mariana Trench in the Pacific, the deepest point on Earth, has its antipode near the Kalahari Desert in Africa. Mount Everest's antipode is in the Pacific Ocean near Easter Island.
Beyond curiosity, antipodal calculations have real applications. In telecommunications, signals sent through Earth's crust (for theoretical point-to-point tunneling) or around the globe (for submarine cables and satellite routing) need to account for maximum distance calculations. Seismologists study how seismic waves from earthquakes focus at the antipodal point — after a major earthquake, sensitive instruments at the antipode can detect focused energy. In amateur radio, "long path" propagation around the back of the globe to reach near-antipodal stations is a well-known technique.
An antipode (or antipodal point) is the point on Earth's surface that is diametrically opposite to a given location. It's. Use antipode coordinates as a directional check, then verify with a geolocation source. where you'd end up if you tunneled straight through the center of the Earth.
Most likely yes. About 71% of Earth's surface is water, and the distribution of land means only roughly 4% of land has a land antipode. Notable land-to-land antipodes include Spain↔New Zealand and parts of South America↔Southeast Asia.
The antipode is always the farthest point from you on Earth's surface. The great-circle distance is approximately 20,015 km (half of Earth's. Review coordinate assumptions before using outputs in any operational planning. circumference), and the straight-line distance through Earth is about 12,742 km.
The antipode is 12 hours different in longitude (180° opposite), so the time zone difference is typically close to ±12 hours, though actual time zones don't follow longitude lines precisely. Confirm hemisphere and timezone context before applying these values practically.
No! The antipode of most US locations is in the Indian Ocean. China's antipode is in South America (Argentina/Chile). The "dig to China" myth doesn't hold geographically.
Very few major cities are true antipodes. The closest pairing is Madrid, Spain and Wellington, New Zealand. Other near-antipodal pairs include Bermuda↔Perth, and Taipei↔Asunción, Paraguay.