Sunset Radiance FieldEarth radius instrument
Earth radius— km
Local image analysis
Calibrated horizon-dip method

Measure Earth from one photograph.

Upload a clear sea horizon. The tool finds the line and reads useful photo metadata; you answer the remaining questions in plain language.

Calculated resultR =km
Attach a clear sea-horizon photo

No known Earth-radius value is used as an input.

01 / Image analysis

Visible horizon

02 / Three answers

Complete the measurement

0/3 ready
Was the camera level when the photo was taken?
“Assume level” is valid only when level was verified while taking the photo. A small unnoticed tilt can turn the answer into kilometres instead of thousands of kilometres. Positive tilt points upward; negative points downward.
  • Horizon extracted from the photo
  • Camera height supplied
  • Lens calibrated
  • Camera level answered
Advanced precision and refraction

Optional. Add known measurement precision to produce a more honest radius range.

The result is computed from your height and the angular dip between true horizontal and the detected horizon. It is never replaced with the accepted Earth radius. A broad Earth-scale sanity check rejects broken calibration instead of presenting it as Earth's radius.

Measurement boundary

The photo supplies the visible horizon and radiance field. Height, lens calibration, camera level, lens distortion, and atmospheric refraction cannot always be inferred from pixels. A level assumption is clearly marked because it directly affects the result, and a non-Earth-scale output is rejected as failed calibration.