How Eratosthenes Measured Earth’s Size

How Eratosthenes Measured Earth’s Size

More than 2,200 years ago, a Greek scholar named Eratosthenes managed to estimate the size of Earth using shadows, geometry, and distance measurements. No satellites. No telescopes. No airplanes.

His answer was surprisingly close to the modern value.

The basic idea was simple. If Earth is curved, then sunlight should hit different places at slightly different angles. By measuring that angle difference between two cities and knowing the distance between them, Eratosthenes could estimate Earth’s entire circumference.

It sounds almost too neat to be real, but the physics behind it is solid. The experiment is still one of the best examples of how careful observation and geometry can reveal something enormous about the world.

The method also mattered historically. It helped move Earth from being a philosophical idea into something measurable.

Who Was Eratosthenes?


Eratosthenes teaching in Alexandria by Bernardo Strozzi (1635)

Eratosthenes teaching in Alexandria by Bernardo Strozzi (1635)

Eratosthenes lived around 276 to 194 BCE and worked in Alexandria, Egypt, one of the major intellectual centers of the ancient world. He was a mathematician, astronomer, geographer, and the chief librarian at the famous Library of Alexandria.

He worked on:

  • geography
  • maps
  • astronomy
  • prime numbers
  • calendars

The Earth measurement experiment is the thing he is most famous for today, but he was already considered one of the smartest scholars of his time.

What makes this experiment special is not just the answer. It is the reasoning behind it.

He realized that shadows could reveal Earth’s curvature.

The Key Observation in Syene

The experiment depended on an observation from the city of Syene, which is modern-day Aswan in southern Egypt.

At local noon on the summer solstice, people noticed something unusual:

  • deep wells were illuminated all the way to the bottom
  • vertical objects cast almost no shadow

That only happens when the Sun is nearly directly overhead.

Eratosthenes compared this with Alexandria, a city farther north. At the exact same moment, vertical objects there still cast shadows.

That difference became the entire foundation of the calculation.

Why the Shadows Were Different

The explanation only works if Earth is curved.

If sunlight reaches Earth as nearly parallel rays, then a curved surface causes different locations to face the Sun at slightly different angles.

That means:

  • one city can have the Sun overhead
  • another city can see the Sun slightly tilted
  • the angle difference reflects Earth’s curvature

Eratosthenes measured this angle in Alexandria using a vertical stick called a gnomon.

The shadow showed an angle of about 7.2 degrees.

That number matters because:

  • a full circle is 360 degrees
  • 7.2 degrees is 1/50 of 360

So Eratosthenes concluded that the distance between Alexandria and Syene must represent roughly 1/50 of Earth’s total circumference.

That is the entire geometric trick.

How the Geometry Worked

Imagine Earth as a sphere.

Now imagine two lines extending from Earth’s center:

  • one to Alexandria
  • one to Syene

The angle between those two lines should match the angle difference of sunlight measured at the surface.

Since the measured angle was about 7.2 degrees:

The distance from Syrene and Alexandria was 5000 stadia (~800 km)

This distance subtended an angle of 7.2 degrees at the center of the Earth.

So how much “distance” will subtend an angle of 360 degree?

This is a direct application of arc geometry.

The difficult part was not the math. The difficult part was measuring the distance accurately.

How Did He Know the Distance Between the Cities?

This part is often oversimplified in modern retellings.

Eratosthenes probably did not personally measure the distance himself. Historians believe he relied on professional surveyors known as bematists.

These surveyors estimated distances by:

  • counting steps
  • measuring caravan travel routes
  • using pacing methods developed for long-distance land measurement

Ancient sources suggest the distance between Alexandria and Syene was taken as about 5,000 stadia.

The exact modern conversion is tricky because historians still debate which “stadion” unit Eratosthenes used.

Different ancient regions used different stadium lengths.

This creates uncertainty in the final result.

What Result Did Eratosthenes Get?

The distance from Syrene and Alexandria was 5000 stadia (~800 km)

  • 7.2 deg subtended by ~800 km
  • 360 deg subtended by 800 / 7.2 * 360

= ~40,000 km

The modern equatorial circumference of Earth is about:

  • 40,075 km

Some interpretations of Eratosthenes’ stadion produce an error of only a few percent.

That is remarkably accurate for around 240 BCE.

Why the Experiment Worked So Well

Several things aligned in Eratosthenes’ favor.

Sunlight Reaching Earth Is Nearly Parallel

The Sun is extremely far away compared to Earth’s size.

Because of that, sunlight rays arriving at Earth are almost parallel. This allows angle differences to represent Earth’s curvature directly.

If the Sun were much closer, the geometry would not work the same way.

The Cities Were Roughly North-South

Syene and Alexandria are not perfectly aligned north-to-south, but they are close enough for a reasonable approximation.

A stronger east-west offset would have complicated the measurement.

Large Distances Reduce Error

The farther apart the cities are, the easier it becomes to measure meaningful angular differences.

Tiny distances would create very small shadow changes and larger percentage errors.

Common Misconceptions About the Experiment

The Sun Was Not Perfectly Overhead in Syene

Many simplified explanations claim the Sun was exactly overhead at Syene.

In reality, modern measurements show Syene is slightly north of the Tropic of Cancer today. Also, Earth’s axial tilt changes slowly over time.

The Sun may have been extremely close to overhead during Eratosthenes’ era, but probably not perfectly centered.

The experiment still works because the error is small.

Earth Was Not “Proven Round” By This Experiment

Educated Greeks already had strong reasons to think Earth was spherical before Eratosthenes.

Earlier thinkers had noticed:

  • curved Earth shadows during lunar eclipses
  • changing star positions with latitude
  • ships disappearing hull-first over the horizon

What Eratosthenes did was measure Earth’s size, not discover that Earth was round.

The Distance Measurement Was Probably the Largest Source of Error

Modern discussions often focus on the shadow angle.

But the biggest uncertainty was likely:

  • the exact route distance
  • the stadion length used
  • surveying accuracy

The geometry itself is straightforward and reliable.

Could You Repeat This Experiment Today?

Yes, and people still do.

Schools and science groups regularly recreate the experiment using:

  • sticks
  • synchronized clocks
  • GPS coordinates
  • online communication between cities

The modern version works exactly the same way:

  1. Measure shadow angles at the same time in two locations
  2. Find the angular difference
  3. Measure the surface distance
  4. Scale the result to a full circle

Even with simple tools, the estimate can get surprisingly close to the real value.

You can calculate too, without waiting for Solstice!

Follow these steps:

  1. Choose two distant locations north-south, and measure a stick's height at each.
  2. Use Google Maps to determine the latitude of both locations and find the distance between them (1 deg latitude = 111 km)
  3. Calculate the angle made by the stick’s shadow
  4. Find the angle subtended at earth’s center using the diagram below
Measuring circumference of the Earth yourself

You know the angle subtended at center (A-B). You know the distance between the sticks. Use basic unitary method to find the circumference. (Give a pat on your back if it comes better than Eratosthenes' value)

Why This Experiment Was Historically Important

The deeper importance of the experiment is philosophical as much as scientific.

Eratosthenes showed that:

  • giant planetary properties could be measured from Earth’s surface
  • geometry could describe the physical world
  • observation plus math could outperform speculation

This became part of the foundation of:

  • geography
  • astronomy
  • navigation
  • surveying
  • geodesy

Later, scientists built on the same idea when measuring:

  • distances to the Moon
  • Earth’s shape
  • planetary motion

The experiment also helped establish the idea that Earth is a measurable object, not just a place humans live on.

That shift changed science permanently.

The Engineering Mindset Behind the Experiment

One reason this story still feels modern is because the method resembles real engineering thinking.

Eratosthenes:

  • noticed a strange observation
  • compared two systems
  • identified a measurable difference
  • used geometry to infer a hidden property
  • accepted approximations where necessary

He did not need perfect conditions.

He only needed:

  • a workable model
  • measurable data
  • logical reasoning

That is still how many scientific measurements work today.

A Simple Stick Revealed a Planet

The most fascinating part is probably the scale mismatch.

A tiny shadow on a stick revealed the size of an entire planet.

No one saw Earth from space for another two thousand years. Yet the geometry was already sitting there in sunlight and shadows, waiting for someone to notice what they meant.

And honestly, that is one of the nicest things about science history. Sometimes the biggest discoveries begin with somebody paying attention to something very ordinary.

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