What Became of the Controversial Fourteenth Archimedean Solid, the Pseudo Rhomb-Cuboctahedron?
Livio Zefiro* and Maria Rosa Ardigo'
*Dip.Te.Ris, Universita' di Genova, Italy
Notes
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INTRODUCTION
In his work "De nive sexangula" [1], quoted
in [2], rather surprisingly Johannes Kepler mentioned
fourteen Archimedean solids, unlike the usual thirteen ones. Probably he was
refering to the pseudo rhomb-cuboctahedron, also known as Miller's solids, since
J.C.P. Miller, as reported in [3-5], obtained it accidentally while trying
to build a model of an Archimedean rhomb-cuboctahedron starting from an
incorrect net. Later, such solid was re-discovered many times, i.e. by V.G.
Ashkinuze (so that, consequently, it is also named Miller-Ashkinuze solid),
and sometimes included in the list of the Archimedean solids.
Due to the lack not only of the particular actractiveness
typical of the Archimedean solids, but mainly of vertex-transitivity [3],
the pseudo rhomb-cuboctahedron does not number among the Archimedean solids.
Analogously, its dual, achievable by means of a 45° rotation of one half of
the deltoid-icositetrahedron (dual of the rhomb-cuboctahedron), is merely a pseudo Catalan solid, not being face-transitive.
THE RHOMB-CUBOCTAHEDRON AND ITS ISOMER, THE PSEUDO RHOMB-CUBOCTAHEDRON
Fig.1 - Animation showing the transformation of the rhomb-cuboctahedron
into the pseudo rhomb-cuboctahedron
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Table 1 - Platonic and Archimedean solids compared with their duals | |||||||
Vertices | Faces | Edges | Faces | Vertices | Point Group | ||
Platonic solids | Dual Platonic solids | ||||||
tetrahedron | 4 | 4 | 6 | 4 | 4 | tetrahedron | 43m |
octahedron | 6 | 8 | 12 | 6 | 8 | cube | m3m |
cube | 8 | 6 | 12 | 8 | 6 | octahedron | m3m |
icosahedron | 12 | 20 | 30 | 12 | 20 | dodecahedron | m 3 5 |
dodecahedron | 20 | 12 | 30 | 20 | 12 | icosahedron | m 3 5 |
Archimedean solids | Dual Catalan solids | ||||||
truncated tetrahedron | 12 | 8 | 18 | 12 | 8 | triakis-tetrahedron | 43m |
cuboctahedron | 12 | 14 | 24 | 12 | 14 | rhomb-dodecahedron | m3m |
truncated cube | 24 | 14 | 36 | 24 | 14 | triakis-octahedron | m3m |
truncated octahedron | 24 | 14 | 36 | 24 | 14 | tetrakis-hexahedron | m3m |
rhomb-cuboctahedron | 24 | 26 | 48 | 24 | 26 | deltoid-icositetrahedron | m3m |
truncated cuboctahedron | 48 | 26 | 72 | 48 | 26 | hexakis-octahedron | m3m |
snub cube (chiral) |
24 | 38 | 60 | 24 | 38 |
pentagonal icositetrahedron (chiral) |
432 |
icosidodecahedron | 30 | 32 | 60 | 30 | 32 | rhomb-triacontahedron | m 3 5 |
truncated dodecahedron | 60 | 32 | 90 | 60 | 32 | triakis-icosahedron | m 3 5 |
truncated icosahedron | 60 | 32 | 90 | 60 | 32 | pentakis-dodecahedron | m 3 5 |
rhomb-icosidodecahedron | 60 | 62 | 120 | 60 | 62 | deltoid-hexecontahedron | m 3 5 |
truncated icosidodecahedron | 120 | 62 | 180 | 120 | 62 | hexakis-icosahedron | m 3 5 |
snub dodecahedron (chiral) | 60 | 92 | 150 | 60 | 92 | pentagonal hexecontahedron (chiral) | 235 |
Given two of three values among the number of faces, edges and vertices, the third one
can be obtained by the well-known relation:
The last column of the table reports the crystallographic
point group relative to each pair of dual polyhedra, according to the International notation (or
Hermann-Mauguin notation).
Four out of the thirteen Archimedean solids can be dissected (Fig.2), originating regular-faced polyhedra: according to the nomenclature introduced by Norman W. Johnson [6], the names of the "elementary" polyhedra so obtained are:
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The rhomb-icosidodecahedron has four other
isomers, whereas icosidodecahedron, cuboctahedron and
rhomb-cuboctahedron have only one other isomeric
form. Particularly noteworthy in case of the rhomb-cuboctahedron, since all its solids angles are congruent.
Focusing our attention on the rhomb-cuboctahedron, its dissection into
elementary polyhedra gives an octagonal prism and two square cupolas (Fig.3). A square cupola includes two
parallel polygons, a square and an octagon, connected
by a ring of other eight polygons, where squares alternate to equilateral
triangles. Both squares and triangles of the ring share one side with the
octagon, whereas the opposite side (in case of the squares) or vertex (in case
of the triangles) are shared with the
square parallel to the octagon.
upper square cupola | octagonal prism | lower square cupola |
Fig.3 - Square cupolas and octagonal prism obtained dissecting the
rhomb-cuboctahedron into regular-faced polyhedra |
Fig.4 - Dissection of the rhomb-cuboctahedron in
regular-faced polyhedra, 45° rotation of the lower square cupola and subsequent
reassembly leading to the pseudo rhomb-cuboctahedron.
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In addition to pseudo rhomb-cuboctahedron and Miller's solid, a further name, deriving from Johnson's nomenclature and showing how the solid can be built starting just from regular-faced elementary polyhedra, is elongated square gyrobicupola, since it includes two square cupolas, reciprocally rotated of 45° (gyro) and separated by an octagonal prism, which makes the resulting form more elongated than a square gyrobicupola (if one applies the same nomenclature to the Archimedean solids, an alternative name of the rhomb-cuboctahedron could be elongated square bicupola).
Two nets of the rhomb-cuboctahedron (left) and
pseudo rhomb-cuboctahedron (right) are shown in Fig.5: in
the rhomb-cuboctahedron a square of each cupola is connected, on opposite sides,
to the same square of the octagonal prism, whereas in the pseudo
rhomb-cuboctahedron similar squares, belonging to the two cupolas, are connected (always on opposite
sides) to contiguous squares of the octagonal prism.
Fig.5 - Nets of the rhomb-cuboctahedron (left) and pseudo rhomb-cuboctahedron (right);
clicking here
one can see alternative coloured nets of the two isomers. |
Fig.6 - Rhomb-cuboctahedron (on the left) and pseudo rhomb-cuboctahedron (on the right) drawn with their respective symmetry operators,
namely mirrors, rotation and roto-inversion axes.
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Fig.7 - View along the [001] direction and relative stereographic projection of rhomb-cuboctahedron (upper row) and pseudo rhomb-cuboctahedron (lower row). |
In the Schoenflies notation, D4v is the symbol of the symmetry group
relative to the pseudo-RCO, whereas in the International notation it is
8m2, indicating that the four mirror planes
present in the pseudo-RCO, at 45° from each other, intersect along a line that
is not only a
Orthogonally to the 8-fold rotoinversion axis and symmetrically interposed between the mirrors,
there are also four 2-fold rotation axes. The absence of the centre of symmetry implies that the mirror planes are not orthogonal
to the even-fold rotation axes of the pseudo-RCO.
At this point one can ascertain that in
RCO the action of the symmetry operators makes all the vertices equivalent:
for example, each 3-fold rotation axis, orthogonal to a triangle, relates the
three vertices of the triangle itself.
In pseudo-RCO, on the contrary, only two vertices of each triangle are related by a mirror,
whereas there is no symmetry operator relating the third vertex (the
one at a corner of the square basis of the cupola) to the others.
Therefore, concerning the isomeric couple consisting of RCO and
pseudo-RCO, only RCO is vertex-transitive (like all the other
Archimedean solids). It can be useful to recall the definition given by Peter R. Cromwell [3]:
"A polyhedron is vertex-transitive (or isogonal) if any vertex can be carried to any other by a symmetry operation".
Consequently, the lack of vertex-transitivity is the objective property that,
added to aesthetical reasons, prevents pseudo-RCO from being numbered among the Archimedean solids.
In other words, according to Viktor A. Zalgaller [7]:
"Besides two infinite series of prisms and antiprisms, ... there further
exist only 13 semiregular polyhedra (the bodies of Archimedes). If instead
of the compatibility of the vertices under selfcoincidence of the polyhedron
as a whole, we require only the local commonness of the vertices, then here
one more, the fourteenth, polyhedron exist."
DUALS OF THE RHOMB-CUBOCTAHEDRON AND THE PSEUDO RHOMB-CUBOCTAHEDRON
Fig.8 - Animation showing the transition from the Catalan
deltoid-icositetrahedron, dual of rhomb-cuboctahedron, to the dual of the pseudo
rhomb-cuboctahedron, by a 45° rotation of the lower half of the polyhedron.
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Fig.9 - Steps leading from the dual of
the rhomb-cuboctahedron to the dual of the pseudo rhomb-cuboctahedron, through the 45°
rotation of one half of the polyhedron.
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have
an equal distance from the centre of the respective solid and an identical shape (they are all kite-shaped),
whereas their different features derive from the vertex transitivity of the RCO alone.
The dual of the Archimedean RCO is obviously a Catalan solid, named
deltoid-icositetrahedron (or trapezohedron), belonging to m3m,
the same point group of RCO: by the action of the relative symmetry operators, one face can be related to all the others.
From a crystallographic point of view, the form, made of 24 kite-shaped (or
deltoidal) faces, can be identified by the generalized Miller's indices
The pseudo-RCO and its unnamed dual belong to the same point
group,
8m2, whose symmetry operators
are instead unable to relate one vertex to all the other, in case of
pseudo-RCO, and one face to all the others, in case of its dual.
It follows that the deltoid-icositetrahedron, like all the Catalan solids, is
face-transitive or isohedral (according again to Peter R. Cromwell [3]: "A polyhedron is said to
be face transitive if for any pair of faces, there is a symmetry of the
polyhedron which carries the first face onto the second"), whereas the
dual of the pseudo-RCO is not face transitive: as described in the next chapter, it can be derived from the intersections
of two single forms, having obviously a lower molteplicity.
In Fig.10 the duals of RCO and pseudo RCO are shown with their symmetry operators.
Fig.10 - The
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Fig.11 - View along the [001] direction, and relative stereographic projection,
of the Archimedean deltoid-icositetrahedron, dual of rhomb-cuboctahedron
(upper row), and the dual of pseudo rhomb-cuboctahedron (lower row). |
Fig.12 - Four-coloured net of deltoid-icositetrahedron, dual of
rhomb-cuboctahedron and two-coloured net of the dual of pseudo rhomb-cuboctahedron. |
DECOMPOSITION OF RHOMB-CUBOCTAHEDRON, PSEUDO RHOMB-CUBOCTAHEDRON AND
THEIR DUALS IN SINGLE FORMS
In Fig.13 the dual of the pseudo RCO (central image) is
decomposed into two single forms, an octagonal bipyramid (on the left) and a tetragonal kite-shaped isosceles trapezohedron (or deltohedron)
on the right, both compatible with the
8m2 point group to which also
the pseudo RCO belongs.
Fig.13 - Scale views of the
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Taking a backward step, since both RCO and pseudo-RCO are not face transitive, they can be decomposed (Fig.14) in different single forms that, taking into account the respective m3m and 8m2 point groups, are:
Fig.14 - From the decomposition of a rhomb-cuboctahedron in single
forms (left), one obtains a cube, an octahedron and a rhomb-dodecahedron,
whereas the pseudo rhomb-cuboctahedron (right) gives an octagonal prism,
a pinacoid and two different 4-fold deltohedra (isosceles trapezohedra with
kite-shaped faces). The indices of the two deltohedra are {101} and {111},
if one assumes a monometric set of three orthogonal reference axes. |
It may be interesting to visualize the single forms originating from
the decomposition of RCO, pseudo-RCO and their duals in the different point
groups which are subgroups of m3m
or 8m2 (Fig.15
and Fig.16, respectively).
Decomposition of the rhomb-cuboctahedron and the deltoid-icositetrahedron, its dual, into sets of forms with lower symmetry, belonging to cubic, trigonal, tetragonal and orthorhombic point groups, all subgroups of the m3m point group |
CUBIC POINT GROUPS |
1 cube (6) |
1 cube (6) |
1 cube (6) |
1 cube (6) 2 tetrahedra (4) 1 rhomb-dodecahedron (12) |
1 cube (6) 2 tetrahedra (4) 1 rhomb-dodecahedron (12) |
m3m | 432 | m3 | 43m | 23 |
1 deltoid-icositetrahedron(24) |
1 deltoid-icositetrahedron(24) |
1 deltoid-icositetrahedron(24) |
2 triakis-tetrahedra (12) |
2 triakis-tetrahedra (12) |
TRIGONAL POINT GROUPS |
3 rhombohedra (6) |
3 rhombohedra (6) |
3 rhombohedra (6) |
6 trigonal pyramids (3) |
6 trigonal pyramids (3) |
3m | 3 | 32 | 3m | 3 |
2 rhombohedra (6) |
4 rhombohedra (6) |
4 rhombohedra (6) |
4 trigonal pyramids (3) |
8 trigonal pyramids (3) |
TETRAGONAL POINT
GROUPS |
2 tetragonal bipyramids
(8) |
2 tetragonal bipyramids
(8) |
2 tetragonal bisphenoids
(4) |
2 tetragonal bisphenoids
(4) |
(4/m)mm | 422 | 4m2 | 42m |
1 bipyramid ditetragonal
(16) |
2 tetragonal trapezohedra (8) |
2 tetragonal bisphenoid
(4) |
2 tetragonal bisphenoid
(4) |
4 pyramid tetragonal (4) |
2 tetragonal bipyramids
(8) |
4 bisphenoids (4) |
4 pyramid tetragonal (4) |
4mm | 4/m | 4 | 4 |
2 pyramid ditetragonal (8) 2 pyramid tetragonal (4) |
3 bipyramid tetragonal (8) |
6 tetragonal bisphenoid (4) |
6 pyramid tetragonal (4) |
ORTHORHOMBIC POINT GROUPS
|
1 rhombic bipyramid (8) |
2 rhombic bisphenoids (4) |
2 rhombic pyramids (4) |
mmm | 222 | mm2 |
3 rhombic bipyramid (8) |
6 rhombic bisphenoids (4) |
6 rhombic pyramids (4) |
Fig.17 - Symmetry and forms constituting the rhomb-cuboctahedron and its dual in
all the subgroups of m3m,
except the ones belonging to the monoclinic and triclinic systems. |
The decomposition of the pseudo rhomb-cuboctahedron and its
dual into single forms belonging to point subgroups of
8m2 is shown in
Fig.18.
Decomposition of the pseudo rhomb-cuboctahedron and its dual in sets of forms, with lower symmetry, belonging to subgroups of the 8m2 point group |
2 tetragonal deltohedra
(8) |
2 tetragonal deltohedra
(8) |
4 tetragonal pyramids (4) |
8m2 | 8 | 4 |
1 octagonal bipyramid (16) 1 tetragonal deltohedron (8) |
3 tetragonal deltohedra
(8) |
6 tetragonal pyramids (4) |
2 tetragonal deltohedra
(8) |
4 rhombic bisphenoids (4) |
4 tetragonal pyramids (4) |
4 dihedra (2) |
42*2* | 22*2* | 4mm | mm2 |
2 tetragonal bipyramids
(8) |
4 rhombic bisphenoids (4) |
2 ditetragonal pyramids
(8) |
6 rhombic pyramids (4) |
The asterisks in 42*2* and 22*2* indicates that the horizontal 2-fold axes are rotated 22.5° with respect to their usual orientation in 422 and 222 cristallographic point groups, in accordance with their orientation in the 8m2 point group. Then the (100) faces of the ditetragonal prism, by rotation along the nearest 2-fold axes, is related to the contiguous (110) and (110) faces, placed at 45° from (100) face. Hence, geometrically, the prism is an octagonal prism.
The only subgroups in common between m3m
and 8m2 are:
The list, relative to the eight shared point subgroups, of the single forms (with
their respective multiplicity) deriving from the decomposition of RCO and pseudo-RCO is
reported in Table 2; the analogous list relative to the decomposition of
their duals is reported in Table 3.
POINT GROUPS | RHOMB-CUBOCTAHEDRON
(26 faces) |
PSEUDO RHOMB-CUBOCTAHEDRON (26 faces) |
422 | 2 tetragonal bipyramids (8) | 2 tetragonal deltohedra (8) |
2 tetragonal prisms (4) | 1 ditetragonal prism (8) | |
1 pinacoid (2) | 1 pinacoid (2) | |
4mm | 4 tetragonal pyramid (4) | 4 tetragonal pyramids (4) |
2 tetragonal prisms (4) | 2 tetragonal prisms (4) | |
2 pedions (1) | 2 pedions (1) | |
4 | 4 tetragonal pyramid (4) | 4 tetragonal pyramids (4) |
2 tetragonal prisms (4) | 2 tetragonal prisms (4) | |
2 pedions (1) | 2 pedions (1) | |
222 | 2 rhombic bisphenoids (4) | 4 rhombic bisphenoids (4) |
3 rhombic prisms (4) | 2 rhombic prisms (4) | |
3 pinacoids (2) | 1 pinacoid (2) | |
mm2 | 2 rhombic pyramids (8) | 4 dihedra (2) |
4 dihedra (2) | 2 rhombic pyramids (4) | |
1 prism (4) | 1 rhombic prism (4) | |
2 pinacoids (2) | 2 pinacoids (2) | |
2 pedions (1) | 2 pedions (1) | |
m | 8 dihedra (2) | 8 dihedra (2) |
1 pinacoids (2) | 1 pinacoids (2) | |
8 pedions (1) | 8 pedions (1) | |
2 | 8 sphenoid (2) | 8 sphenoid (2) |
4 pinacoids (2) | 4 pinacoids (2) | |
2 pedions (1) | 2 pedions (1) | |
1 | 26 pedions (1) | 26 pedions (1) |
Table2 - Decomposition in single forms of the rhomb-cuboctahedron and the pseudo rhombcuboctahedron, relatively to the shared subgroups of m3m and 8m2; the multiplicity of each form, namely the number of its faces, is reported in round brackets. |
POINT GROUPS | Dual of the RHOMB-CUBOCTAHEDRON (24 faces) |
Dual of the PSEUDO RHOMB-CUBOCTAHEDRON (24 faces) |
422 | 1 tetragonal bipyramid (8) | 2 tetragonal bipyramids (8) |
2 tetragonal trapezohedra (8) | 1 tetragonal deltohedron (8) | |
4mm | 2 ditetragonal pyramids (8) | 2 ditetragonal pyramids (8) |
2 tetragonal pyramids (4) | 2 tetragonal pyramids (4) | |
4 | 6 tetragonal pyramids (4) | 6 tetragonal pyramids (4) |
222 | 6 rhombic bisphenoids (4) | 4 rhombic bisphenoids (4) |
2 rhombic prisms (4) | ||
mm2 | 6 rhombic pyramids (4) | 6 rhombic pyramids (4) |
m | 12 dihedra (2) | 11 dihedra (2) |
2 pedions(2) | ||
2 | 12 sphenoids (2) | 12 sphenoids (2) |
1 | 24 pedions (1) | 24 pedions (1) |
Table3 - Decomposition in single forms of the duals of
the rhomb-cuboctahedron and the pseudo rhombcuboctahedron, relatively to the
shared subgroups of m3m
and 8m2. |
Symmetry of the rhomb-cuboctahedron in 422 point group and visualization of the constituting forms |
Fig.19 - Rhomb-cuboctahedron (centre) with the rotation axes relative to
the 422 point group; on the left
the |
Symmetry of the pseudo
rhomb-cuboctahedron in 422 point group and visualization of the
constituting
forms |
| |
Fig.20
Upper row: pseudo rhomb-cuboctahedron (left)
with the rotation axes relative to the 422 point group; on the right the Lower row: {111} red tetragonal deltohedron (left) and {101} yellow tetragonal deltohedron (right) Also in this case (and in the following ones) the indices have been calculated assuming a monometric set of three orthogonal reference axes. |
Symmetry of the
dual of the rhomb-cuboctahedron in 422 point group and visualization
of the single constituting forms |
Fig.21
Upper row: dual of the rhomb-cuboctahedron (left) with the simmetry axes relative to
the 422 point group;
on the right the
Lower row: {√2+1 1 1} ochre tetragonal deltohedron (left) and |
Symmetry of the dual of the pseudo
rhomb-cuboctahedron in 422 point group and visualization of the single constituting
forms |
| |
Fig.22
Upper row: the dual of pseudo rhomb-cuboctahedron with the simmetry axes relative to the 422 point group
(left) and the
Lower row: {√2+1 1 1} ochre tetragonal bipyramid (left) and |
In summary, with regard to the isomeric couple RCO-pseudo RCO evaluated in 422
point group, in addition to the two
Concerning the duals, also the
2) C. Hardie
The Six-cornered Snowflake, Oxford University Press, 1966
3)
Peter R. Cromwell
Polyhedra,
Cambridge University Press, 1997
4)
W.W. Rouse Ball, H.S.M. Coxeter
Mathematical Recreations and Essays, Dover Publications,
1987
5)
http://www.georgehart.com/virtual-polyhedra/pseudo-rhombicuboctahedra.html
6) Norman W. Johnson
Convex Polyhedra with Regular Faces, Canadian Journal of Mathematics,
18, 169-200, 1966
7) Viktor A. Zalgaller
Convex Polyhedra with Regular Faces, Seminars in Mathematics - V.A.
Steklov Mathematical Institute, Leningrad - Volume 2, Consultants Bureau, 1969