Long before satellites and laser measuring tools, no one knew how big the Earth was. People guessed, argued, and made wildly different claims. Some thought the planet was enormous; others believed it was much smaller. What they all agreed on was this: the Earth was far too large to measure directly.
Then came Eratosthenes. He lived more than two thousand years ago and worked in the Great Library of Alexandria — a place filled with scrolls, scholars, and a great deal of sunshine. He heard something curious: in a southern city called Syene, the Sun shone straight down a well on the summer solstice. At the very same moment in Alexandria, a vertical stick cast a small shadow.
This tiny difference — the angle of a single shadow — was the clue. Eratosthenes realized he could “slice” the Earth using shadows the same way we slice area under a line: by taking a simple local measurement and using it to understand something much bigger.
In this activity, you will follow the same idea. You start from the angle θ and the distance D between the two cities, compute the ratio R = C / D, and then work your way to Earth’s circumference in meters and kilometers. Finally, you compare your estimate with a present-day value and see how close you came. The angle θ is the fraction of the full circle between the two cities. The ratio R = C / D tells you how many times that distance D fits around the full Earth. From the geometry of the circle, you can use the relationship R = 360° / θ.
Use the diagram to read the value of θ (in degrees). In Eratosthenes’ classic experiment, θ ≈ 7.2°. The distance between Syene and Alexandria along the surface is D meters.
Now use the idea above to compute the ratio R. Remember, R tells you how many times the distance D fits around the entire Earth.
R = 360° / θ
Once you know D (in meters) and R, you can find the Earth’s circumference in meters using:
Circumference in meters = R × D
Then convert to kilometers by dividing by 1000:
Circumference in kilometers = (circumference in meters) ÷ 1000
A commonly used present-day value for Earth’s circumference is about 40,075 kilometers.
First, compute the difference between the present-day value and your estimate:
difference = present-day value − your estimate
Then use this difference to find the percent error of your estimate:
percent error = (difference ÷ present-day value) × 100%