In geometry, a Platonic solid is a convex regular polyhedron. These are the three-dimensional analogs of the regular polygons. There are precisely five such figures (shown below). The name of each figure derives from the number of faces in each — which are 4, 6, 8, 12, and 20 respectively. They are unique in that the sides, edges and angles are all congruent.

(tetrahedron.gif)
(hexahedron.gif)
(octahedron.gif)
(dodecahedron.gif)
(icosahedron.gif)

Tetrahedron	Hexahedron or Cube	Octahedron	Dodecahedron	Icosahedron

Due to their aesthetic beauty and symmetry, the Platonic solids have been a favorite subject of geometers for thousands of years. They are named for the ancient Greek philosopher Plato who claimed the classical elements were constructed from the regular solids.

History

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The five Platonic solids have been known since antiquity. It is unknown who first discovered them. Certainly, all five solids were known to the ancient Greeks. There is evidence, however, that these figures were known long before the time of the Greeks. The neolithic people of Scotland constructed stone models of all five solids at least 1000 years before Plato (Atiyah and Sutcliffe 2003). These models are kept at the Ashmolean Museum in Oxford.

In regards to Greek mathematics, some sources (such as Proclus) credit Pythagoras with the discovery of the five regular solids. Other evidence suggests he may have only been familiar with the tetrahedron, cube and dodecahedron, and that the discovery of the octahedron and icosahedron belong to Theaetetus, a contemporary of Plato. In any case, Theaetetus gave a mathematical description of all five and may have been responsible for the first proof that there exist no more regular solids.

The Platonic solids feature prominently in the philosophy of Plato for whom they are named. Plato wrote about them in the dialogue Timaeus c.360 B.C. in which he associated each of the four classical elements (earth, air, water, and fire) with a regular solid. Earth was associated with the cube, air with the octahedron, water with the icosahedron, and fire with the tetrahedron. There was intuitive justification for these associations: the heat of fire feels sharp and stabbing (like little tetrahedra). Air is made of the octahedron; its minuscule components are so smooth that one can barely feel it. Water, the icosahedron, flows out of one's hand when picked up, as if it is made of tiny little balls. By contrast, a highly un-spherical solid, the hexahedron (cube) represents earth. These clumsy little solids cause dirt to crumble and breaks when picked up, in stark difference to the smooth flow of water. The fifth Platonic solid, the dodecahedron, Plato obscurely remarks, "...the god used for arranging the constellations on the whole heaven". Aristotle added a fifth element, aithêr (aether in Latin, "ether" in English) and postulated that the heavens were made of this element, but he had no interest in matching it with Plato's fifth solid.

Euclid gave a complete mathematical description of the Platonic solids in the Elements; the last book (Book XIII) of which is devoted to their properties. Propositions 13–17 in Book XIII describe the construction of the tetrahedron, octahedron, cube, icosahedron, and dodecahedron in that order. For each solid Euclid finds the ratio of the diameter of the circumscribed sphere to the edge length. In Proposition 18 he argues that there are no further regular solids. Much of the information in Book XIII is probably derived from the work of Theaetetus.

In the 16th century, the German astronomer Johannes Kepler attempted to find a relation between the five known planets at that time (excluding the Earth) and the five regular solids. In Mysterium Cosmographicum, published in 1596, Kepler laid out a model of the solar system in which the five solids were set inside one another and separated by a series of inscribed and circumscribed spheres. The six spheres each corresponded to one of the planets (Mercury, Venus, Earth, Mars, Jupiter, and Saturn). The solids were ordered with the innermost being the octahedron, followed by the icosahedron, dodecahedron, tetrahedron, and finally the cube. In this way the structure of the solar system and the distance relationships between the planets was dictated by the Platonic solids. In the end, Kepler's original idea had to be abandoned, but out of his research came the discovery of the Kepler solids, the realization that the orbits of planets are not circles, and Kepler's laws of planetary motion for which he is now famous.

Combinatorical properties

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A convex polyhedron is regular if and only if

1. all its faces are congruent regular polygons, and
2. the same number of faces meet at each of its vertices.

Each Platonic solid can therefore be denoted by a symbol {p, q} where

p = the number of sides of each face (or the number of vertices of each face) and

q = the number of faces meeting at each vertex (or the number of edges meeting at each vertex).

The symbol {p, q}, called the Schläfli symbol, gives a combinatorical description of the polyhedron. The Schläfli symbols of the five Platonic solids are given in the table below.

Polyhedron		Faces	Edges	Vertices	Schläfli symbol	Vertex configuration
tetrahedron	4	6	4	{3, 3}	3.3.3
cube	6	12	8	{4, 3}	4.4.4
octahedron	8	12	6	{3, 4}	3.3.3.3
dodecahedron	12	30	20	{5, 3}	5.5.5
icosahedron	20	30	12	{3, 5}	3.3.3.3.3

All other combinatorical information about these solids, such as total number of faces (F), edges (E), and vertices (V), can be determined from p and q. Since any edge joins two vertices and has two adjacent faces we must have:

$pF\; =\; 2E\; =\; qV.\backslash ,$

The other relationship between these values is given by Euler's formula:

$F\; -\; E\; +\; V\; =\; 2.\backslash ,$

This nontrivial fact can be proved in a great variety of ways (in algebraic topology it follows from the fact that the Euler characteristic of the sphere is 2). Together these three relationships completely determine F, E, and V:

$F\; =\; \backslash frac\{4q\}\{4\; -\; (p-2)(q-2)\},\backslash quad\; E\; =\; \backslash frac\{2pq\}\{4\; -\; (p-2)(q-2)\},\backslash quad$

V = \frac{4p}{4 - (p-2)(q-2)}. Note that swapping p and q interchanges F and V while leaving E unchanged (For a geometric interpretation of this fact see the section on dual polyhedra below).

Classification

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The limitation to five regular solids is easily demonstrated using elementary geometry:

1. Each vertex of the solid must coincide with one vertex each of at least three faces.
2. At each vertex of the solid, the total, among the adjacent faces, of the angles between their respective adjacent sides must be less than 360°.
3. The angles at all vertices of all faces of a Platonic solid are identical, so each vertex of each face must contribute less than 360°/3=120°.
4. Regular polygons of six or more sides have only angles of 120° or more, so the common face must be the triangle, square, or pentagon. And for:
   • Triangular faces: each vertex of a regular triangle is 60°, so a shape may have 3, 4, or 5 triangles meeting at a vertex; these are the tetrahedron, octahedron, and icosahedron respectively.
   • Square faces: each vertex of a square is 90°, so there is only one arrangement possible with three faces at a vertex, the cube.
   • Pentagonal faces: each vertex is 108°; again, only one arrangement, of three faces at a vertex is possible, the dodecahedron.

A purely topological (rather than geometric) proof can be made using only combinatorical information about the solids. The key is Euler's formula, $F-E+V\; =\; 2$, and the fact that $pF\; =\; 2E\; =\; qV$. Combining these equations one obtains the equation

$\backslash frac\{2E\}\{p\}\; -\; E\; +\; \backslash frac\{2E\}\{q\}\; =\; 2.$

Therefore

$2E\backslash left(\{1\backslash over\; p\}+\{1\backslash over\; q\}\backslash right)\; =\; E\; +\; 2$

or

$\{1\backslash over\; p\}+\{1\backslash over\; q\}\; =\; \{1\backslash over\; 2\}\; +\; \{1\backslash over\; E\}.$

Since $E$ is strictly positive we must have

$\backslash frac\{1\}\{p\}\; +\; \backslash frac\{1\}\{q\}\; >\; \backslash frac\{1\}\{2\}.$

Using the fact that p and q must both be at least 3, one can easily see that there are only five possibilities for {p, q}:

$\backslash \{3,\; 3\backslash \},\backslash quad\; \backslash \{4,\; 3\backslash \},\backslash quad\; \backslash \{3,\; 4\backslash \},\backslash quad\; \backslash \{5,\; 3\backslash \},\backslash quad\; \backslash \{3,5\backslash \}.$

Both of the above proofs only show that there can be no more than five regular solids. That all five actually exist is a separate question — one that can be answered by an explicit construction.

Symmetry

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Dual polyhedra

Every polyhedron has a dual polyhedron with faces and vertices interchanged. The dual of every Platonic solid is another Platonic solid, so that we can arrange the five solids into dual pairs.

• The tetrahedron is self-dual (i.e. its dual is another tetrahedron).
• The cube and the octahedron form a dual pair.
• The dodecahedron and the icosahedron form a dual pair.

One can construct the dual polyhedron by taking the vertices of the dual to be the centers of the faces of the original figure. The edges of the dual are formed by connecting the centers of adjacent faces in the original. In this way, the number of faces and vertices is interchanged, while the number of edges stays the same.

If a polyhedron has Schläfli symbol {p, q}, then its dual has the symbol {q, p}. Indeed every combinatorical property of one Platonic solid can be interpreted as another combinatorical property of the dual.

Symmetry groups

In mathematics, the concept of symmetry is studied with the notion of a mathematical group. Every polyhedron has an associated symmetry group, which is the set of all transformations (Euclidean isometries) which leave the polyhedron invariant. The order of the symmetry group is the number of symmetries of the polyhedron. One often distinguishes between the full symmetry group, which includes reflections, and the proper symmetry group, which includes only rotations.

The symmetry groups of the Platonic solids are known as polyhedral groups (which are a special class of the point groups in three dimensions). The high degree of symmetry of the Platonic solids can be interpreted in a number of ways. Most importantly, the vertices of each solid are all equivalent under the action of the symmetry group, as are the edges and faces. One says the action of the symmetry group is transitive on the vertices, edges, and faces. In fact, this is another way of defining regularity of a polyhedron: a polyhedron is regular if and only if it is vertex-uniform, edge-uniform, and face-uniform.

There are only three symmetry groups associated with the Platonic solids rather than five, since the symmetry group of any polyhedron coincides with that of its dual. This is easily seen by examing the construction of the dual polyhedron. Any symmetry of the original must be a symmetry of the dual and vice-versa. The three polyhedral groups are:

• the tetrahedral group T,
• the octahedral group O (which is also the symmetry group of the cube), and
• the icosahedral group I (which is also the symmetry group of the dodecahedron).

The orders of the proper (rotation) groups are 12, 24, and 60 respectively — precisely twice the number of edges in the respective polyhedra. The orders of the full symmetry groups are twice as much again (24, 48, and 120). See (Coxeter 1973) for a derivation of these facts.

The following table lists the various symmetry properties of the Platonic solids. The symmetry groups listed are the full groups with the rotation subgroups given in parenthesis (likewise for the number of symmetries). Wythoff's kaleidoscope construction is a method for constructing polyhedra directly from their symmetry groups. We list for reference Wythoff's symbol for each of the Platonic solids.

Polyhedron	Schläfli symbol	Wythoff symbol	Dual polyhedron	Symmetries	Symmetry group
tetrahedron	{3, 3}	3 > 2 3	tetrahedron	24 (12)	Td (T)
cube	{4, 3}	3 > 2 4	octahedron	48 (24)	Oh (O)
octahedron	{3, 4}	4 > 2 3	cube
dodecahedron	{5, 3}	3 > 2 5	icosahedron	120 (60)	Ih (I)
icosahedron	{3, 5}	5 > 2 3	dodecahedron

Geometric properties

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There are a number of angles associated with each Platonic solid. The dihedral angle is the interior angle between any two face planes. The dihedral angle, θ, of the solid {p,q} is given by the formula

$\backslash sin\{\backslash theta\backslash over\; 2\}\; =\; \backslash frac\{\backslash cos(\backslash pi/q)\}\{\backslash sin(\backslash pi/p)\}.$

This is sometimes more conveniently expressed in terms of the tangent by

$\backslash tan\{\backslash theta\backslash over\; 2\}\; =\; \backslash frac\{\backslash cos(\backslash pi/q)\}\{\backslash sin(\backslash pi/h)\}.$

The quantity h is 4, 6, 6, 10, and 10 for the tetrahedron, cube, octahedron, dodecahedron, and icosahedron respectively.

The angular deficiency at the vertex of a polyhedron is the difference between the sum of the face-angles at that vertex and 2π. The defect, δ, at any vertex of the regular polyhedra {p,q} is

$\backslash delta\; =\; 2\backslash pi\; -\; q\backslash pi\backslash left(1-\{2\backslash over\; p\}\backslash right).$

By Descartes' theorem, this is equal to 4π divided by the number of vertices (i.e. the total defect at all verticies is 4π).

The 3-dimensional analog of a plane angle is a solid angle. The solid angle, Ω, at the vertex of a regular polyhedron is given in terms of the dihedral angle by

$\backslash Omega\; =\; q\backslash theta\; -\; (q-2)\backslash pi.\backslash ,$

This follows from the spherical excess formula for a spherical polygon and the fact that the vertex figure of the polyhedron {p,q} is a regular q-gon.

The various angles associated with the Platonic solids are tabulated below. The numerical values of the solid angles are given in steradians. The constant φ = (1+√5)/2 is the golden ratio.

Polyhedron	Dihedral angle $(\backslash theta)\backslash ,$	$\backslash tan\backslash frac\{\backslash theta\}\{2\}$	Defect $(\backslash delta)\backslash ,$	Solid angle $(\backslash Omega)\backslash ,$
tetrahedron	70.53°	$1\backslash over\{\backslash sqrt\; 2\}$	$\backslash pi\backslash ,$	$2\backslash tan^\{-1\}\backslash left(\backslash frac\{\backslash sqrt\; 2\}\{5\}\backslash right)$	$\backslash approx\; 0.551286$
cube	90°	$1\backslash ,$	$\backslash pi\backslash over\; 2$	$\backslash frac\{\backslash pi\}\{2\}$	$\backslash approx\; 1.57080$
octahedron	109.47°	$\backslash sqrt\; 2$	$\{2\backslash pi\}\backslash over\; 3$	$4\backslash sin^\{-1\}\backslash left(\{1\backslash over\; 3\}\backslash right)$	$\backslash approx\; 1.35935$
dodecahedron	116.56°	$\backslash varphi\backslash ,$	$\backslash pi\backslash over\; 5$	$2\backslash tan^\{-1\}\backslash varphi^5$	$\backslash approx\; 2.96174$
icosahedron	138.19°	$\backslash varphi^2\backslash ,$	$\backslash pi\backslash over\; 3$	$2\backslash pi\; -\; 5\backslash sin^\{-1\}\backslash left(\{2\backslash over\; 3\}\backslash right)$	$\backslash approx\; 2.63455$

Another virtue of regularity is that the Platonic solids all possess three concentric spheres:

• the circumscribed sphere which passes through all the vertices,
• the midsphere which is tangent to each edge at the midpoint of the edge, and
• the inscribed sphere which is tangent to each face at the center of the face.

The radii of these spheres are called the circumradius, the midradius, and the inradius. These are the distances from the center of the polyhedron to the vertices, edge midpoints, and face centers respectively. The circumradius R and the inradius r of the solid {p, q} with edge length a are given by

$R\; =\; \backslash left(\{a\backslash over\; 2\}\backslash right)\backslash tan\backslash frac\{\backslash pi\}\{q\}\backslash tan\backslash frac\{\backslash theta\}\{2\}$

$r\; =\; \backslash left(\{a\backslash over\; 2\}\backslash right)\backslash cot\backslash frac\{\backslash pi\}\{p\}\backslash tan\backslash frac\{\backslash theta\}\{2\}$

where θ is the dihedral angle. The midradius ρ is given by

$\backslash rho\; =\; \backslash left(\{a\backslash over\; 2\}\backslash right)\backslash frac\{\backslash cos(\backslash pi/p)\}\{\backslash sin(\backslash pi/h)\}$

where h is the quantity used above in the definition of the dihedral angle (h = 4, 6, 6, 10, or 10). Note that the ratio of the circumradius to the inradius is symmetric in p and q:

$\{R\backslash over\; r\}\; =\; \backslash tan\backslash frac\{\backslash pi\}\{p\}\backslash tan\backslash frac\{\backslash pi\}\{q\}.$

The surface area, A, of a regular polyhedron {p, q} is easily computed as area of a regular p-gon times the number of faces F. This is:

$A\; =\; \backslash left(\{a\backslash over\; 2\}\backslash right)^2\; Fp\backslash cot\backslash frac\{\backslash pi\}\{p\}.$

The volume is computed as F times the volume of the pyramid whose base is a regular p-gon and whose height is the inradius r. That is,

$V\; =\; \{1\backslash over\; 3\}rA.$

In the following table we list the various radii of the Platonic solids together with their surface area and volume. The overall size is fixed by taking the edge length, a, to be equal to 2.

Polyhedron (a = 2)	r	ρ	R	A	V
tetrahedron	$1\backslash over\; \{\backslash sqrt\; 6\}$	$1\backslash over\; \{\backslash sqrt\; 2\}$	$\backslash sqrt\{3\backslash over\; 2\}$	$4\backslash sqrt\; 3$	$\backslash frac\{2\backslash sqrt\; 2\}\{3\}$
cube	$1\backslash ,$	$\backslash sqrt\; 2$	$\backslash sqrt\; 3$	$24\backslash ,$	$8\backslash ,$
octahedron	$\backslash sqrt\{2\backslash over\; 3\}$	$1\backslash ,$	$\backslash sqrt\; 2$	$8\backslash sqrt\; 3$	$\backslash frac\{8\backslash sqrt\; 2\}\{3\}$
dodecahedron	$\backslash frac\{\backslash varphi^2\}\{\backslash xi\}$	$\backslash varphi^2$	$\backslash sqrt\; 3\backslash ,\backslash varphi$	$60\backslash frac\{\backslash varphi\}\{\backslash xi\}$	$20\backslash frac\{\backslash varphi^3\}\{\backslash xi^2\}$
icosahedron	$\backslash frac\{\backslash varphi^2\}\{\backslash sqrt\; 3\}$	$\backslash varphi$	$\backslash xi\backslash varphi$	$20\backslash sqrt\; 3$	$\backslash frac\{20\backslash varphi^2\}\{3\}$

The constants φ and ξ in the above are given by

$\backslash varphi\; =\; 2\backslash cos\{\backslash pi\backslash over\; 5\}\; =\; \backslash frac\{1+\backslash sqrt\; 5\}\{2\}\backslash qquad\backslash xi\; =\; 2\backslash sin\{\backslash pi\backslash over\; 5\}\; =\; \backslash sqrt\{\backslash frac\{5-\backslash sqrt\; 5\}\{2\}\}\; =\; 5^\{1/4\}\backslash varphi^\{-1/2\}.$

Among the Platonic solids, either the dodecahedron or the icosahedron may be seen as the best approximation to the sphere. The icosahedron has the largest number of faces, the largest dihedral angle, and it hugs its inscribed sphere the tightest. The dodecahedron, on the other hand, has the smallest angular defect, the largest vertex solid angle, and it fills out its circumscribed sphere the most.

In nature and technology

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The tetrahedron, cube, and octahedron all occur naturally in crystal structures. These by no means exhaust the numbers of possible forms of crystals. However, neither the regular icosahedron nor the regular dodecahedron are amongst them. One of the forms, called the pyritohedron (named for the group of minerals of which it is typical) has twelve pentagonal faces, arranged in the same pattern as the faces of the regular dodecahedron. The faces of the pyritohedron are, however, not regular, so the pyritohedron is also not regular.

In the early 20th century, Ernst Haeckel described (Haeckel, 1904) a number of species of Radiolaria, some of whose skeletons are shaped like various regular polyhedra. Examples include Circoporus octahedrus, Circogonia icosahedra, Lithocubus geometricus and Circorrhegma dodecahedra. The shapes of these creatures should be obvious from their names.

Many viruses, such as the herpes virus, have the shape of a regular icosahedron. Viral structures are built of repeated identical protein subunits and the icosahedron is the easiest shape to assemble using these subunits. A regular polyhedron is used because it can be built from a single basic unit protein used over and over again; this saves space in the viral genome.

In meteorology and climatology, global numerical models of atmospheric flow are of increasing interest which employ grids that are based on an icosahedron (refined by triangulation) instead of the more commonly used longitude/latitude grid. This has the advantage of evenly distributed spatial resolution without singularities (i.e. the poles) at the expense of somewhat greater numerical difficulty.

Geometry of space frames is often based on platonic solids. In MERO system, Platonic solids are used for naming convention of various space frame configurations. For example ½O+T refers to a configuration made of one half of octahedron and a tetrahedron.

Platonic solids are often used to make dice, because dice of these shapes can be made fair. 6-sided dice are very common, but the other numbers are commonly used in role-playing games. Such dice are commonly referred to as dn where n is the number of faces (d8, d20, etc.); see dice notation for more details. These shapes frequently show up in other games or puzzles. Puzzles similar to a Rubik's Cube come in all five shapes — see magic polyhedra.

Related polyhedra and polytopes

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There exist 4 regular polyhedra which are not convex, called Kepler-Poinsot solids. These all have icosahedral symmetry and may be obtained as stellations of the dodecahedron and the icosahedron.

cuboctahedron
icosidodecahedron The next most regular convex polyhedra after the Platonic solids are the cuboctahedron, which is a rectification of the cube and the octahedron, and the icosidodecahedron, which is a rectification of the dodecahedron and the icosahedron (the rectification of the self-dual tetrahedron is a regular octahedron). These are both quasi-regular meaning that they are vertex- and edge-uniform and have regular faces, but the faces are not all congruent (coming in two different classes). They form 2 of the 13 Archimedean solids, which are the convex semi-regular polyhedra with polyhedral symmetry.

The uniform polyhedra form a much broader class of polyhedra. These figures are vertex-uniform and have regular or star polygons for faces. These include all the polyhedra mentioned above together with an infinte set of prisms, antiprisms, and 53 other non-convex forms. The Johnson solids are convex polyhedra which have regular faces but are not uniform.

The 3 regular tessellations of the plane are closely related to the Platonic solids. Indeed, one can view the Platonic solids as the 5 regular tessellations of the sphere. This is done by projecting each solid onto a concentric sphere. The faces project onto regular spherical polygons which exactly cover the sphere. One can show that every regular tessellation of the sphere is characterized by a pair of integers {p, q} with 1/p + 1/q > 1/2. Likewise, a regular tessellation of the plane is characterized the condition 1/p + 1/q = 1/2. There are three possibilities:

• {4, 4} which a square tiling,
• {3, 6} which is a triangular tiling, and
• {6, 3} which is a hexagonal tiling (dual to the triangular tiling).

In a similar manner one can consider regular tessellations of the hyperbolic plane. These are characterized the condition 1/p + 1/q < 1/2. There are an infinite number of such tessellations.

Moving to higher dimensions, polyhedra are generalized to polytopes. In the mid-19th century the Swiss mathematician Ludwig Schläfli discovered the four-dimensional analogs of the Platonic solids, called convex regular 4-polytopes. There are exactly 6 of these figures; 5 of which are generalizations of the Platonic solids and a sixth one, the 24-cell, which has no lower dimensional analog.

In dimensions higher than four, there are only 3 convex regular polytopes: the simplex, the measure polytope, and the cross-polytope. In three dimensions, these coincide with the tetrahedron, the cube, and the octahedron.

See also

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• Regular polytopes
• List of regular polytopes

References

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• Haeckel, E. (1904). Kunstformen der Natur. Available as Haeckel, E. (1998); Art forms in nature, Prestel USA. ISBN 3791319906, or online at ^*.

External links

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• Book XIII of Euclid's Elements.
• Interactive 3D Polyhedra in Java
• Platonic Solids Interactive animation.

Platonic solids | Polyhedra

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