Stand on a hilltop and sight the horizon. The taller the hill, the further the horizon dips below level.
The sightline just touches the Earth, at right angles to its radius. That right triangle links the hill, the dip and the Earth’s radius.
Whose hill:
The Earth in cross-section at one fixed scale · the model hills are far taller than real ones, so the angle is big enough to see
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THE IDEAThe dip at the summit equals the angle at the Earth’s centre. With the hill’s height h, the right triangle gives R = h × cos(dip) ÷ (1 − cos(dip)).
The person behind the ideas
Studied astronomy, geography and the sciences of India.
Worked in Khwarazm and later in Ghazna.
Connected careful measurements with geometric calculations.
More of the mathematics
Measuring the hill first
From the plain, he sighted the summit from two places in line with it and measured the distance between them. Two angles and that distance give the height, even when the hill’s foot cannot be reached.
A tiny angle, a big effect
His dip was just over half a degree. Reading it 1′ differently changes the answer by about 6%, so the instrument had to be read with great care.