Find the geometric horizon distance from observer height and planetary radius.
Calculate horizon distance
Enter eye height above the surface and use Earth's mean radius or another planet radius.
About distance to the horizon
The horizon is the apparent boundary where a curved planetary surface blocks the direct line of sight. As an observer rises above the surface, the tangent point moves farther away and the visible horizon expands. This calculator models the observer, planet center, and tangent point as a right triangle. It uses d = √(2Rh + h²), where d is straight-line distance to the horizon, R is planetary radius, and h is observer height above the surface. The calculator converts the entered radius to meters, evaluates the exact geometric equation, and reports kilometers.
For heights that are very small compared with Earth's radius, the h² term contributes little and the familiar approximation d ≈ √(2Rh) works well. At an eye height of two meters on a smooth spherical Earth, the geometric horizon is about 5.05 kilometers away. At one hundred meters it is about 35.70 kilometers away. Horizon range grows with the square root of height, so doubling observer height does not double viewing distance. To double geometric range, height must increase by roughly a factor of four.
The result represents the direct tangent line, not distance measured along the curved surface. At ordinary terrestrial heights those values are close, but they diverge at great altitude. The model also treats the body as a perfect sphere. Earth is an oblate spheroid, and local curvature varies with latitude and viewing direction. Mountains, waves, buildings, trees, and elevation of the target can alter what is actually visible. If both observer and target are elevated, calculate each one's horizon distance and add them for an approximate maximum line-of-sight separation.
Atmospheric refraction usually bends light slightly toward Earth's surface and can extend the optical horizon beyond the purely geometric value. Weather gradients can increase, decrease, or distort that effect, while radio propagation often uses an effective Earth-radius model. This tool deliberately reports the uncorrected geometric baseline so assumptions remain clear. It is useful for navigation intuition, photography planning, tower sight lines, astronomy, and classroom geometry. Do not use a simple horizon estimate as the sole basis for maritime navigation, radio engineering, aviation separation, or safety-critical visibility decisions.
Horizon distance examples
Observer and body
Distance
Typical viewpoint
2 m above Earth, radius 6,371 km
5.048 km
Standing observer
100 m above Earth, radius 6,371 km
35.696 km
Observation tower
10,000 m above Earth, radius 6,371 km
357.099 km
High-altitude aircraft
How to calculate horizon distance
Measure the observer's eye or sensor height above the local surface.
Enter that height in meters.
Keep the mean Earth radius or enter the radius of another spherical body.
Select Calculate horizon distance and account separately for terrain or refraction.
Frequently asked questions
What formula calculates distance to the horizon?
The exact spherical formula is d = √(2Rh + h²). It comes from the right triangle formed by the planet center, observer, and tangent point.
Why does height have a square-root effect?
At normal heights, the dominant relationship is d ≈ √(2Rh). Therefore range increases more slowly than observer height.
Does atmospheric refraction change the result?
Yes, standard refraction commonly extends the visible optical horizon. Actual refraction varies with atmospheric temperature and density gradients.
How do I include an elevated target?
Calculate the horizon distance for the observer and target separately. Add the two results for an approximate maximum mutual line-of-sight range.
Is Earth really a sphere with radius 6,371 km?
That value is a useful mean radius for general estimates. Precise work should use local curvature, terrain, and an ellipsoidal Earth model.