JF Ptak Science Books Post 1193
[This pamphlet may be purchased from our blog bookstore site, here.]
This is the first of a few short essays of the idea of pre-historic appearances of important ideas. I use the word “pre-historic” in its literal sense—that is, these papers were published before the concepts that they discussed were recognized and published, later, in more complete form and of course to greater fame. One will certainly be Gregor Mendl’s paper (Versuche über Plflanzenhybriden ) published in the obscure Verhandlungen des naturforschenden Vereines in Brünn, (Brno), and to be resurrected at the hands of Gregory Bateson thirty-odd years later to much acclaim. Another example is Vannevar Bush’s “As We May Think”, published in The Atlantic Monthly in June 1945, and which was a now widely recognized definite intellectual precursor to the construction of what we know today as the Internet.
Right now, though, I’d like to look at the pre-birth of fractals in Benoit Mandelbrot’s precursor (1967) paper (and in a weird, probably not-correct way, scooping himself) to his more famous effort of 1975, in which he coins the term and fully describes "fractals", showing the measurement of the coastlines behave like a fractal over a range of measurement scales.
The seminal paper, How Long Is the Coast of Britain? Statistical Self-Similarity and Fractional Dimension, published in Science magazine in 1967, is an introduction to the concept of fractals (which Mandelbrot would name later in 1975). The kernel of it all is found in the Lewis Fry Richardson graphs and more so in the small illustration on page three of the paper—the peek into the future world of fractals, seeing a fractal before it was named so.
Richardson (a kind of Jevons, or Marey-like American figure on the history of 20th century science) did some very good thinking about the elusive nature of naming such a thing as the lengths of coastlines and other natural constructions: namely he determined that their measured length was dependent upon the scale of measurement. That is to say the measured length, L(G), is ruled the scale of G, approximating the function as L(G)=M(G)1-0
Mandelbrot moves on to discuss the coastline in terms of it being a self-similar object, which is something that is nearly exactly similar to a part of itself, or the whole having the same shape of one or more than one of its parts, and regresses.
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