Map global paths from coordinates and sphere radius. View bearings, midpoint, angles, and travel estimates. Fast results help pilots, sailors, students, and curious explorers.
| Route | Start Coordinates | End Coordinates | Radius | Speed | Use Case |
|---|---|---|---|---|---|
| New York to London | 40.7128, -74.0060 | 51.5074, -0.1278 | 6371 km | 900 km/h | Flight planning example |
| Tokyo to Sydney | 35.6762, 139.6503 | -33.8688, 151.2093 | 6371 km | 850 km/h | Long-distance route study |
| Moon rover path | 12.5000, 18.2000 | -4.1000, 45.9000 | 1737.4 km | 12 km/h | Spherical surface modeling |
This calculator uses spherical geometry. A great circle is the shortest path between two points on a sphere. It is useful in navigation, geophysics, astronomy, and route analysis.
a = sin²(Δφ / 2) + cos(φ₁) · cos(φ₂) · sin²(Δλ / 2)
c = 2 · asin(√a)
d = R · c
chord = 2R · sin(c / 2)
θ = atan2[sin(Δλ) · cos(φ₂), cos(φ₁) · sin(φ₂) − sin(φ₁) · cos(φ₂) · cos(Δλ)]
The midpoint is computed from spherical vector relationships using both coordinates and the longitudinal difference.
Here, φ is latitude in radians, λ is longitude in radians, Δ means difference, and R is the chosen sphere radius.
A great circle is any circle on a sphere whose center matches the sphere’s center. It gives the shortest surface route between two points on that sphere.
Flat maps distort the curved surface of a sphere. Great circle distance follows spherical geometry, so it is usually more accurate for global travel and physics-based surface calculations.
Yes. Enter the proper mean radius for any spherical body, such as Mars or the Moon. The calculator then returns distance and chord values for that chosen sphere.
Use any consistent unit for radius, such as kilometers, miles, meters, or nautical miles. The returned distance and chord length will match that same unit.
The initial bearing is the starting direction you would follow from the first point along the great circle path. It is measured clockwise from geographic north.
On a sphere, the route curves relative to latitude and longitude lines. Because of that curvature, the arrival direction at the destination often differs from the starting direction.
Chord length is the straight line through the sphere between two surface points. It helps compare surface travel distance with internal straight-line separation.
It is excellent for spherical modeling and education. For highest Earth accuracy, professional geodesy usually uses an ellipsoidal model instead of a perfect sphere.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.