In geometry, a dodecahedron is a polyhedron with twelve flat faces. The most well-known is the regular dodecahedron, one of the Platonic solids, featuring regular pentagonal faces and icosahedral symmetry of order 120. There are also star shapes like the small stellated and great stellated dodecahedra formed by stellations. Variants like the pyritohedron and tetartoid have different symmetries, while the rhombic dodecahedron exhibits octahedral symmetry and is notable for its space-filling properties. Many dodecahedra share combinatorial structure but differ in face shape and symmetry.
Regular dodecahedron
Main article: Regular dodecahedron
The convex regular dodecahedron is one of the five regular Platonic solids and can be represented by its Schläfli symbol {5,3}.
The dual polyhedron is the regular icosahedron {3,5}, having five equilateral triangles around each vertex.
Four kinds of regular dodecahedra| Convex regular dodecahedron | Small stellated dodecahedron | Great dodecahedron | Great stellated dodecahedron |
The convex regular dodecahedron also has three stellations, all of which are regular star dodecahedra. They form three of the four Kepler–Poinsot polyhedra. They are the small stellated dodecahedron {5/2,5}, the great dodecahedron {5,5/2}, and the great stellated dodecahedron {5/2,3}. The small stellated dodecahedron and great dodecahedron are dual to each other; the great stellated dodecahedron is dual to the great icosahedron {3,5/2}. All of these regular star dodecahedra have regular pentagonal or pentagrammic faces. The convex regular dodecahedron and great stellated dodecahedron are different realisations of the same abstract regular polyhedron; the small stellated dodecahedron and great dodecahedron are different realisations of another abstract regular polyhedron.
Other pentagonal dodecahedra
In crystallography, two important dodecahedra can occur as crystal forms in some symmetry classes of the cubic crystal system that are topologically equivalent to the regular dodecahedron but less symmetrical: the pyritohedron with pyritohedral symmetry, and the tetartoid with tetrahedral symmetry:
Pyritohedron
| Pyritohedron | |
|---|---|
| (See here for a rotating model.) | |
| Face polygon | isosceles pentagon |
| Coxeter diagrams | |
| Faces | 12 |
| Edges | 30 (6 + 24) |
| Vertices | 20 (8 + 12) |
| Symmetry group | Th, [4,3+], (3*2), order 24 |
| Rotation group | T, [3,3]+, (332), order 12 |
| Dual polyhedron | Pseudoicosahedron |
| Properties | face transitive |
| Net | |
A pyritohedron is a dodecahedron with pyritohedral (Th) symmetry. Like the regular dodecahedron, it has twelve identical pentagonal faces, with three meeting in each of the 20 vertices (see figure).3 However, the pentagons are not constrained to be regular, and the underlying atomic arrangement has no true fivefold symmetry axis. Its 30 edges are divided into two sets – containing 24 and 6 edges of the same length. The only axes of rotational symmetry are three mutually perpendicular twofold axes and four threefold axes.
Although regular dodecahedra do not exist in crystals, the pyritohedron form occurs in the crystals of the mineral pyrite, and it may be an inspiration for the discovery of the regular Platonic solid form. The true regular dodecahedron can occur as a shape for quasicrystals (such as holmium–magnesium–zinc quasicrystal) with icosahedral symmetry, which includes true fivefold rotation axes.
Crystal pyrite
The name crystal pyrite comes from one of the two common crystal habits shown by pyrite (the other one being the cube). In pyritohedral pyrite, the faces have a Miller index of (210), which means that the dihedral angle is 2·arctan(2) ≈ 126.87° and each pentagonal face has one angle of approximately 121.6° in between two angles of approximately 106.6° and opposite two angles of approximately 102.6°. The following formulas show the measurements for the face of a perfect crystal (which is rarely found in nature).
Height = 5 2 ⋅ Long side {\displaystyle {\text{Height}}={\frac {\sqrt {5}}{2}}\cdot {\text{Long side}}}
Width = 4 3 ⋅ Long side {\displaystyle {\text{Width}}={\frac {4}{3}}\cdot {\text{Long side}}}
Short sides = 7 12 ⋅ Long side {\displaystyle {\text{Short sides}}={\sqrt {\frac {7}{12}}}\cdot {\text{Long side}}}
Cartesian coordinates
The eight vertices of a cube have the coordinates (±1, ±1, ±1).
The coordinates of the 12 additional vertices are (0, ±(1 + h), ±(1 − h2)), (±(1 + h), ±(1 − h2), 0) and (±(1 − h2), 0, ±(1 + h)).
h is the height of the wedge-shaped "roof" above the faces of that cube with edge length 2.
An important case is h = 1/2 (a quarter of the cube edge length) for perfect natural pyrite (also the pyritohedron in the Weaire–Phelan structure).
Another one is h = 1/φ = 0.618... for the regular dodecahedron. See section Geometric freedom for other cases.
Two pyritohedra with swapped nonzero coordinates are in dual positions to each other like the dodecahedra in the compound of two dodecahedra.
| Animations | |
|---|---|
| Honeycomb of alternating convex and concave pyritohedra with heights between ±1/φ | Heights between 0 (cube)and 1 (rhombic dodecahedron) |
Geometric freedom
The pyritohedron has a geometric degree of freedom with limiting cases of a cubic convex hull at one limit of collinear edges, and a rhombic dodecahedron as the other limit as 6 edges are degenerated to length zero. The regular dodecahedron represents a special intermediate case where all edges and angles are equal.
It is possible to go past these limiting cases, creating concave or nonconvex pyritohedra. The endo-dodecahedron is concave and equilateral; it can tessellate space with the convex regular dodecahedron. Continuing from there in that direction, we pass through a degenerate case where twelve vertices coincide in the centre, and on to the regular great stellated dodecahedron where all edges and angles are equal again, and the faces have been distorted into regular pentagrams. On the other side, past the rhombic dodecahedron, we get a nonconvex equilateral dodecahedron with fish-shaped self-intersecting equilateral pentagonal faces.
| Special cases of the pyritohedron | |||||||
|---|---|---|---|---|---|---|---|
| Versions with equal absolute values and opposing signs form a honeycomb together. (Compare this animation.)The ratio shown is that of edge lengths, namely those in a set of 24 (touching cube vertices) to those in a set of 6 (corresponding to cube faces). | |||||||
| Ratio | 1 : 1 | 0 : 1 | 1 : 1 | 2 : 1 | 1 : 1 | 0 : 1 | 1 : 1 |
| h | −√5 + 1/2 | −1 | −√5 + 1/2 | 0 | √5 − 1/2 | 1 | √5 + 1/2 |
| −1.618... | −0.618... | 0.618... | 1.618... | ||||
| Image | Regular star, great stellated dodecahedron, with regular pentagram faces | Degenerate, 12 vertices in the center | The concave equilateral dodecahedron, called an endo-dodecahedron. | A cube can be divided into a pyritohedron by bisecting all the edges, and faces in alternate directions. | A regular dodecahedron is an intermediate case with equal edge lengths. | A rhombic dodecahedron is a degenerate case with the 6 crossedges reduced to length zero. | Self-intersecting equilateral dodecahedron |
Tetartoid
| TetartoidTetragonal pentagonal dodecahedron | |
|---|---|
| (See here for a rotating model.) | |
| Face polygon | irregular pentagon |
| Conway notation | gT |
| Faces | 12 |
| Edges | 30 (6+12+12) |
| Vertices | 20 (4+4+12) |
| Symmetry group | T, [3,3]+, (332), order 12 |
| Properties | convex, face transitive |
A tetartoid (also tetragonal pentagonal dodecahedron, pentagon-tritetrahedron, and tetrahedric pentagon dodecahedron) is a dodecahedron with chiral tetrahedral symmetry (T). Like the regular dodecahedron, it has twelve identical pentagonal faces, with three meeting in each of the 20 vertices. However, the pentagons are not regular and the figure has no fivefold symmetry axes.
Although regular dodecahedra do not exist in crystals, the tetartoid form does. The name tetartoid comes from the Greek root for one-fourth because it has one fourth of full octahedral symmetry, and half of pyritohedral symmetry.4 The mineral cobaltite can have this symmetry form.5
Abstractions sharing the solid's topology and symmetry can be created from the cube and the tetrahedron. In the cube each face is bisected by a slanted edge. In the tetrahedron each edge is trisected, and each of the new vertices connected to a face center. (In Conway polyhedron notation this is a gyro tetrahedron.)
| Relationship to the dyakis dodecahedron | ||
|---|---|---|
A tetartoid can be created by enlarging 12 of the 24 faces of a dyakis dodecahedron.(The tetartoid shown here is based on one that is itself created by enlarging 24 of the 48 faces of the disdyakis dodecahedron.) The crystal model on the right shows a tetartoid created by enlarging the blue faces of the dyakis dodecahedral core. Therefore, the edges between the blue faces are covered by the red skeleton edges. |
Cartesian coordinates
The following points are vertices of a tetartoid pentagon under tetrahedral symmetry:
(a, b, c); (−a, −b, c); (−n/d1, −n/d1, n/d1); (−c, −a, b); (−n/d2, n/d2, n/d2),under the following conditions:6
0 ≤ a ≤ b ≤ c, n = a2c − bc2, d1 = a2 − ab + b2 + ac − 2bc, d2 = a2 + ab + b2 − ac − 2bc, nd1d2 ≠ 0.Geometric freedom
The regular dodecahedron is a tetartoid with more than the required symmetry. The triakis tetrahedron is a degenerate case with 12 zero-length edges. (In terms of the colors used above this means, that the white vertices and green edges are absorbed by the green vertices.)
| Tetartoid variations from regular dodecahedron to triakis tetrahedron | |||||||
|---|---|---|---|---|---|---|---|
Dual of triangular gyrobianticupola
A lower symmetry form of the regular dodecahedron can be constructed as the dual of a polyhedron constructed from two triangular anticupola connected base-to-base, called a triangular gyrobianticupola. It has D3d symmetry, order 12. It has 2 sets of 3 identical pentagons on the top and bottom, connected 6 pentagons around the sides which alternate upwards and downwards. This form has a hexagonal cross-section and identical copies can be connected as a partial hexagonal honeycomb, but all vertices will not match.
Rhombic dodecahedron
The rhombic dodecahedron is a zonohedron with twelve rhombic faces and octahedral symmetry. It is dual to the quasiregular cuboctahedron (an Archimedean solid) and occurs in nature as a crystal form. The rhombic dodecahedron packs together to fill space.
The rhombic dodecahedron can be seen as a degenerate pyritohedron where the 6 special edges have been reduced to zero length, reducing the pentagons into rhombic faces.
The rhombic dodecahedron has several stellations, the first of which is also a parallelohedral spacefiller.
Another important rhombic dodecahedron, the Bilinski dodecahedron, has twelve faces congruent to those of the rhombic triacontahedron, i.e. the diagonals are in the ratio of the golden ratio. It is also a zonohedron and was described by Bilinski in 1960.7 This figure is another spacefiller, and can also occur in non-periodic spacefillings along with the rhombic triacontahedron, the rhombic icosahedron and rhombic hexahedra.8
Other dodecahedra
There are 6,384,634 topologically distinct convex dodecahedra, excluding mirror images—the number of vertices ranges from 8 to 20.9 (Two polyhedra are "topologically distinct" if they have intrinsically different arrangements of faces and vertices, such that it is impossible to distort one into the other simply by changing the lengths of edges or the angles between edges or faces.)
Topologically distinct dodecahedra (excluding pentagonal and rhombic forms)
- Uniform polyhedra:
- Decagonal prism – 10 squares, 2 decagons, D10h symmetry, order 40.
- Pentagonal antiprism – 10 equilateral triangles, 2 pentagons, D5d symmetry, order 20
- Johnson solids (regular faced):
- Pentagonal cupola – 5 triangles, 5 squares, 1 pentagon, 1 decagon, C5v symmetry, order 10
- Snub disphenoid – 12 triangles, D2d, order 8
- Elongated square dipyramid – 8 triangles and 4 squares, D4h symmetry, order 16
- Metabidiminished icosahedron – 10 triangles and 2 pentagons, C2v symmetry, order 4
- Congruent irregular faced: (face-transitive)
- Hexagonal bipyramid – 12 isosceles triangles, dual of hexagonal prism, D6h symmetry, order 24
- Hexagonal trapezohedron – 12 kites, dual of hexagonal antiprism, D6d symmetry, order 24
- Triakis tetrahedron – 12 isosceles triangles, dual of truncated tetrahedron, Td symmetry, order 24
- Other less regular faced:
- Hendecagonal pyramid – 11 isosceles triangles and 1 regular hendecagon, C11v, order 11
- Trapezo-rhombic dodecahedron – 6 rhombi, 6 trapezoids – dual of triangular orthobicupola, D3h symmetry, order 12
- Rhombo-hexagonal dodecahedron or elongated Dodecahedron – 8 rhombi and 4 equilateral hexagons, D4h symmetry, order 16
- Truncated pentagonal trapezohedron, D5d, order 20, topologically equivalent to regular dodecahedron
Practical usage
Armand Spitz used a dodecahedron as the "globe" equivalent for his Digital Dome planetarium projector,10 based upon a suggestion from Albert Einstein.
Regular dodecahedrons are sometimes used as dice, when they are known as d12s, especially in games such as Dungeons and Dragons.
See also
- 120-cell – a regular polychoron (4D polytope) whose surface consists of 120 dodecahedral cells
- Braarudosphaera bigelowii – a dodecahedron shaped coccolithophore (a unicellular phytoplankton algae)
- Pentakis dodecahedron
- Roman dodecahedron
- Snub dodecahedron
- Truncated dodecahedron
External links
Wikimedia Commons has media related to Polyhedra with 12 faces.- Plato's Fourth Solid and the "Pyritohedron", by Paul Stephenson, 1993, The Mathematical Gazette, Vol. 77, No. 479 (Jul., 1993), pp. 220–226 [1]
- Stellation of Pyritohedron VRML models and animations of Pyritohedron and its stellations
- Klitzing, Richard. "3D convex uniform polyhedra o3o5x – doe".
- Editable printable net of a dodecahedron with interactive 3D view
- The Uniform Polyhedra
- Origami Polyhedra – Models made with Modular Origami
- Virtual Reality Polyhedra The Encyclopedia of Polyhedra
- K.J.M. MacLean, A Geometric Analysis of the Five Platonic Solids and Other Semi-Regular Polyhedra
- Dodecahedron 3D Visualization
- Stella: Polyhedron Navigator: Software used to create some of the images on this page.
- How to make a dodecahedron from a Styrofoam cube
References
1908 Chambers's Twentieth Century Dictionary of the English Language, 1913 Webster's Revised Unabridged Dictionary ↩
Athreya, Jayadev S.; Aulicino, David; Hooper, W. Patrick (May 27, 2020). "Platonic Solids and High Genus Covers of Lattice Surfaces". Experimental Mathematics. 31 (3): 847–877. arXiv:1811.04131. doi:10.1080/10586458.2020.1712564. S2CID 119318080. https://www.tandfonline.com/doi/abs/10.1080/10586458.2020.1712564 ↩
Crystal Habit. Galleries.com. Retrieved on 2016-12-02. http://www.galleries.com/minerals/property/crystal.htm#dodecahe ↩
Dutch, Steve. The 48 Special Crystal Forms Archived 2013-09-18 at the Wayback Machine. Natural and Applied Sciences, University of Wisconsin-Green Bay, U.S. https://www.uwgb.edu/dutchs/symmetry/xlforms.htm ↩
Crystal Habit. Galleries.com. Retrieved on 2016-12-02. http://www.galleries.com/minerals/property/crystal.htm#dodecahe ↩
The Tetartoid. Demonstrations.wolfram.com. Retrieved on 2016-12-02. http://demonstrations.wolfram.com/TheTetartoid/ ↩
Hafner, I. and Zitko, T. Introduction to golden rhombic polyhedra. Faculty of Electrical Engineering, University of Ljubljana, Slovenia. http://www.mi.sanu.ac.rs/vismath/hafner2/IntrodRhombic.html ↩
Lord, E. A.; Ranganathan, S.; Kulkarni, U. D. (2000). "Tilings, coverings, clusters and quasicrystals". Curr. Sci. 78: 64–72. http://met.iisc.ernet.in/~lord/webfiles/tcq.html ↩
Counting polyhedra. Numericana.com (2001-12-31). Retrieved on 2016-12-02. http://www.numericana.com/data/polycount.htm ↩
Ley, Willy (February 1965). "Forerunners of the Planetarium". For Your Information. Galaxy Science Fiction. pp. 87–98. https://archive.org/stream/Galaxy_v23n03_1965-02#page/n87/mode/2up ↩