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Mathematics 1967

How Long Is the Coast of Britain?

Benoit B. Mandelbrot

Measure a coastline with a finer ruler and it only grows longer — its real “length” is a fractional dimension.

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In depth · the introduction

Ask how long Britain's coastline is, and the honest answer is: it depends on your ruler — and the finer the ruler, the longer the coast, with no end in sight.

The idea, unpacked

Measure a coast with a long ruler and you skip over the small bays and headlands, getting a modest length. Switch to a shorter ruler and you trace into those bays — and the bays have smaller bays, which have smaller bays still. Every time you shrink the ruler you catch more wrinkles, and the total length grows. It never settles down.

So “how long is it?” has no single answer. What does have an answer is how fast the length grows as the ruler shrinks — and that rate is a number Mandelbrot called the dimension. A straight line scores 1; the more crinkled the curve, the higher above 1 it climbs. Britain's rugged west coast comes out around 1.25.

Where it came from

The puzzle had been hiding in plain sight. Years earlier the meteorologist Lewis Fry Richardson, studying what makes nations go to war, noticed that reference books disagreed wildly about the length of the border between Spain and Portugal — because each had measured with a different ruler. He collected the data and found a clean pattern in it, but died before making much of it. Benoit Mandelbrot, a restless mathematician at IBM with a taste for problems others thought beneath them, picked it up, saw that the pattern meant a kind of dimension, and in 1967 published it under a title that sounds like a child's question. Years later he gave the whole subject its name: fractals.

Why it mattered

For two thousand years geometry had been about smooth, ideal shapes — lines, circles, spheres — the things nature almost never makes. Coastlines, mountains, clouds, trees, rivers and lungs are rough, broken and branching, and the old geometry had no honest way to describe them. This paper offered one: measure the roughness with a fractional dimension. It turned “rugged” from a vague impression into a quantity you can compute and compare.

A shape that is all coast

Picture a snowflake's edge built by a simple rule: take a line, push a triangular bump out of its middle third, then do the same to every new edge, forever. Zoom in anywhere and you see the same bumps on bumps on bumps — the edge looks equally crinkly at every magnification. A real coastline behaves the same way: a piece of it, enlarged, resembles the whole. Try shrinking the ruler yourself below and watch the length climb.

A crinkly coastline that looks the same at every zoom level. As you move the slider to a smaller ruler, the curve grows more detailed and the measured-length number climbs higher and higher, while a dimension readout stays near 1.26 — the curve's roughness.

Where it sits

This is the moment geometry made room for nature's roughness. It descends from Euclid's smooth figures (also in this Library) by rebelling against them, and it shares a border with chaos theory: the strange attractors Edward Lorenz found in 1963 are fractals too. A decade on, the same arithmetic produced the Mandelbrot set, the most famous picture in mathematics — and the fractal terrains of every modern video game.

The original document
Original source text
B. B. Mandelbrot · Science, New Series, 156(3775): 636–638 · May 5, 1967
The question
Geographical curves are so involved in their detail that their lengths are often infinite or, more accurately, undefinable.
Measure a coastline on a map and you get one number; measure the same coast with a smaller ruler that catches every bay and headland and you get a larger one — and the number keeps climbing as the ruler shrinks, with no length to settle on.
Statistical self-similarity
The paper's resolution is that many natural curves are statistically self-similar: each piece, suitably magnified, looks like a reduced-scale image of the whole, so a coastline carries the same kind of detail at every scale rather than smoothing out.
A fractional dimension
Mandelbrot takes Lewis Fry Richardson's empirical observation — that measured length grows as a power of the ruler size, L(ε) ∝ ε^(1−D) — and reinterprets the exponent D as a dimension. For a smooth curve D = 1; for the rugged west coast of Britain Richardson's data give D ≈ 1.25; a gentler coast such as South Africa's sits near 1.02. D measures roughness.
[ … ]
Source
The complete three-page paper — with Richardson's data and the self-similar constructions — is available in full at the source below. The word “fractal” itself came later, in Mandelbrot's 1975 essay.
IBM Research · 1967