5 Fractal Geometry
5.1 Natural Geometry, Self-similarity and Fractal Dimension
Classical geometry typically considers objects (lines, curves, spheres, etc.) which seem flatter and
less interesting as one zooms in: a differentiable curve at small scales 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 it greater due to the
dimples? What if we zoom in further? Under a microscope, the dimples 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 the 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? Round every grain of sand?
Every molecule? As one shrinks the scale, the measured length becomes absurdly large. We sketch
Mandelbrot’s approach.
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• Given a ruler of length R, measure how many N are required to trace round the coastline when
laid end-to-end.
• Plotting log N against log(1/R) for several sizes of ruler seems to give 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.
Mandelbrot’s fractal dimension is purely empirical, though it does seem to capture something about
the ‘bumpiness’ of a coastline: the bumpier, 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 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 1.
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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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