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A coastline has no single true length, because the finer you measure it the longer it gets
A coastline has no single true length, because the closer you measure it the longer it becomes. Coastlines are jagged at every scale, from hundreds of kilometres down to fractions of a millimetre, so there is no smallest feature that should count. A ruler measuring a metal bar gets closer to the true answer as its precision improves, but a shorter ruler on a coast just traces more bays and pebbles and keeps adding length. Lewis Fry Richardson first studied the effect systematically, and Benoit Mandelbrot later showed that the mathematics of fractals explains it. The true length is therefore undefined, not just unknown.
Measuring a coast means laying a line of fixed step length along it. A small step follows every inlet and headland, adding length that a larger step would skip. Because coastlines are fractal, the number of new details keeps growing as the step shrinks, so the total grows without limit rather than converging to one value.
The paradox shows that some everyday measurements are only meaningful once you specify a scale, which matters for mapping borders, coastal planning and science. It is also a foundational idea behind fractal geometry, which describes many natural shapes such as clouds, rivers and lungs.
Mandelbrot's 1967 paper 'How Long Is the Coast of Britain?' was published in the journal Science.
From Wikipedia, the free encyclopedia · text CC BY-SA 4.0
Illustrative photo · Vyacheslav Argenberg, CC BY 4.0, via Wikimedia Commons
