Pinwheel Tiling
Visualization
AIFS program
@
$dim=2
s=$companion([1,0])
r=[-1,0,0,1]
g=2+s^3
h0=s^3*r*[2,0]
h1=[0,1]
h2=s^2*[2,-2]
h3=s^2*r*[0,-1]
h4=s^2*r*[-2,-2]
A=g^-1*(h0|h1|h2|h3|h4)*A
Overview
The Pinwheel Tiling was discovered by John Conway and formalized by Charles Radin (1994). Its prototile is the right triangle with legs 1 and 2 (hypotenuse ), which decomposes into five congruent smaller copies scaled by — an integer Moran ratio .
The defining feature of the pinwheel tiling is rotational ergodicity: every orientation of the tile appears in the tiling with equal statistical frequency. No translational symmetry exists. This puts the pinwheel in a class of its own among aperiodic substitution tilings.
The same algebraic framework ( in , five maps contracting by ) also supports two fractal single-tile variants with a fractal boundary, discovered by Bandt and Mekhontsev via computer search (2019).
Classical Pinwheel (Radin, 1994)
The classical tile is the solid 1-2- right triangle. The five maps partition the triangle exactly — their images cover the whole tile with pairwise intersections of measure zero. The IFS attractor is therefore a solid triangular region.
The tiling is non-periodic: the group of symmetries of the tiling contains no translations or rotations. Yet Radin proved that the frequency of tiles in each orientation is uniform over the full circle — every angle appears equally often. This “statistical” rotational symmetry is the pinwheel’s most remarkable property.
Conway and Radin extended the construction to three dimensions: the quaquaversal tiling uses a single tetrahedral tile such that every 3D orientation appears equally.
Fractal Single-Tile Pinwheel (Bandt & Mekhontsev)
An exhaustive computer search (Mekhontsev, 2019) over all five-map IFS with expansion and maps drawn from the group generated by and revealed that exactly two substitutions produce a non-periodic tiling with dense tile orientations using a single prototile with a fractal boundary. Both are shown below.
Like the classical tile, each fractal variant is a substitution tile: the five images of the attractor under the maps cover exactly, with pairwise intersections of measure zero. The attractor is a compact, connected, simply-connected set whose boundary has Hausdorff dimension strictly between 1 and 2 — in contrast to the straight edges of the classical triangle.
The existence of such a tile was not previously known; Frank and Whittaker (2011) had constructed a fractal version of the pinwheel tiling using 13 prototiles via a theoretical approach, but the one-tile version required a computer search.
Algebraic Structure
Both variants share the same algebraic object. In the Gaussian integers , the expansion is:
In matrix form (using for rotation and for -axis reflection):
The characteristic polynomial is , with roots .
All three tiles satisfy with the same , , , but different translation vectors:
| Map | Classical | Fractal 1 | Fractal 2 |
|---|---|---|---|
The maps are isometries from composed with integer translations, with .
References
- Radin, C. (1994). The pinwheel tilings of the plane. Annals of Mathematics, 139(3), 661–702.
- Conway, J. H. & Radin, C. (1998). Quaquaversal tilings and rotations. Inventiones Mathematicae, 132(1), 179–188.
- Bandt, C., Mekhontsev, D. & Tetenov, A. (2018). A single fractal pinwheel tile. Proceedings of the American Mathematical Society, 146(3), 1271–1285.
- Frank, N. P. & Whittaker, M. F. (2011). A fractal version of the pinwheel tiling. The Mathematical Intelligencer, 33(2), 7–17.
- Pinwheel tiling — Wikipedia
- Pinwheel — Tilings Encyclopedia
- Fractal Single-Tile Pinwheel — Tilings Encyclopedia
- Mekhontsev, D. (2019). An algebraic framework for finding and analyzing self-affine tiles and fractals.