
5 Fractal Geometry
5.1 Natural Geometry, Self-similarity and Fractal Dimension
The objects of classical geometry (lines, curves, spheres, etc.) tend to seem flatter and less interesting
as one zooms in: at small scales, every differentiable curve looks like a line segment! By contrast,
real-world objects tend to exhibit greater detail at smaller scales. A seemingly spherical orange is
dimpled on closer inspection: is its surface area that of a sphere, or is the area greater due to the
dimples? What if we zoom in further? Under a microscope, the dimples in the orange are seen to
have minute cracks and fissures. With modern technology, we can ‘see’ almost to the molecular level;
what does surface area even mean at such a scale?
The Length of a Coastline In 1967 Benoit Mandelbrot asked a related question in a now-famous
paper, How Long Is the Coast of Britain? Statistical Self-Similarity and Fractional Dimension. His essential
point was that this question has no simple answer:
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Should one measure by walking along the mean
high tide line? But where is this? Do we ‘walk’ round every pebble? Do we skirt every grain of sand?
Every molecule? As the scale of consideration shrinks, the measured length becomes absurdly large.
Here is a sketch of Mandelbrot’s approach.
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• Given a ruler of length R, let N be the number required to trace round the coastline when laid
end-to-end.
• Plot log N against log(1/R) for several sizes of ruler. The data suggests a straight line!
log N ≈ log k + D log(1/R) = log(kR
−D
) =⇒ N ≈ kR
−D
The number D is Mandelbrot’s fractal dimension of the coastline.
This notion of fractal dimension is purely empirical, though it does seem to capture something about
the ‘roughness’ of a coastline: the bumpier the coast, the greater its fractal dimension. For mainland
Britain with its smooth east and rugged west coasts D ≈ 1.25. Given its many fjords, Norway has a
far rougher coastline and thus a higher fractal dimension D ≈ 1.52.
Example 5.1. As a sanity check, consider a smooth circular ‘coastline.’
Approximate the circumference using N rulers of length R: clearly
R = 2 sin
π
N
As N → ∞, the small angle approximation for sine applies,
R ≈
2π
N
=⇒ N ≈ 2π R
−1
where the approximation improves as N → ∞. The fractal dimension of a circle is therefore D = 1.
The same analysis applies to any smooth curve (Exercise 3).
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The official answer from the Ordnance Survey (the UK government mapping office) is, ‘It depends.’ The all-knowing
CIA states 7723 miles, though offers no evidence as to why.
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For more detail see the Fractal Foundation’s website. Mandelbrot coined the word fractal, though he didn’t invent the
concept from nothing. Rather he applied earlier ideas of Hausdorff, Minkowski and others, and observed how the natural
world contains many examples of fractal structures.
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