A fractal is a geometric shape containing detailed structure at arbitrarily small scales, usually with a fractal dimension that strictly exceeds its topological dimension. Many fractals look similar across different scales, a property called self-similarity, and if the replication is exactly identical at every scale, as in the Menger sponge, the shape is called affine self-similar; fractal geometry connects to measure theory through the Hausdorff dimension. Fractals differ from ordinary geometric figures in how they scale: doubling the edge lengths of a filled polygon multiplies its area by four, two raised to its dimension of two, while doubling a fractal's one-dimensional lengths scales its spatial content by a power that need not be an integer, called the fractal dimension. Starting from notions of recursion in the seventeenth century, fractals developed through the nineteenth-century study of continuous but nowhere-differentiable functions by Bernard Bolzano, Bernhard Riemann and Karl Weierstrass, to the coining of the word fractal by Benoit Mandelbrot in the twentieth century, who in 1982 defined a fractal as a set whose Hausdorff-Besicovitch dimension strictly exceeds its topological dimension before later broadening the definition to a rough or fragmented shape splittable into parts that are each an approximate reduced copy of the whole.
Facts
Origin YearYear marks Mandelbrot coining the term itself; precursor mathematical objects now recognized as fractals go back to Weierstrass (1872) and Cantor (1883) per the same article History section. Connections
Sources
1. Fractal (Wikipedia)
Wikimedia FoundationLead section
In mathematics, a fractal is a geometric shape containing detailed structure at arbitrarily small scales, usually having a fractal dimension strictly exceeding the topological dimension.
Etymology section, term coined
The term "fractal" was coined by the mathematician Benoit Mandelbrot in 1975.
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