Bipyramid

 ( Polyhedra ) 

In geometry, a bipyramid, dipyramid, or double pyramid is a polyhedron formed by fusing two pyramids together base-to-base. The base of each pyramid must therefore be the same, and unless otherwise specified the base vertices are usually coplanar and a bipyramid is usually symmetric, meaning the two pyramids are across their common base plane. When each apex (, the off-base vertices) of the bipyramid is on a line perpendicular to the base and passing through its center, it is a right bipyramid; otherwise it is oblique. When the base is a regular polygon, the bipyramid is also called regular.

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Definition and properties A bipyramid is a polyhedron constructed by fusing two pyramids which share the same base; a pyramid is in turn constructed by connecting each vertex of its base to a single new vertex (the apex) not lying in the plane of the base, for an gonal base forming triangular faces in addition to the base face. An gonal bipyramid thus has faces, edges, and vertices. More generally, a right pyramid is a pyramid where the apices are on the perpendicular line through the centroid of an arbitrary polygon or the incenter of a tangential polygon, depending on the source. Likewise, a right bipyramid is a polyhedron constructed by attaching two symmetrical right bipyramid bases; bipyramids whose apices are not on this line are called oblique bipyramids.

When the two pyramids are mirror images, the bipyramid is called symmetric. It is called regular if its base is a regular polygon. When the base is a regular polygon and the apices are on the perpendicular line through its center (a regular right bipyramid) then all of its faces are isosceles triangles; sometimes the name bipyramid refers specifically to symmetric regular right bipyramids, Examples of such bipyramids are the triangular bipyramid, octahedron (square bipyramid) and pentagonal bipyramid. If all their edges are equal in length, these shapes consist of equilateral triangle faces, making them deltahedron; the triangular bipyramid and the pentagonal bipyramid are , and the regular octahedron is a Platonic solid.

The symmetric regular right bipyramids have prismatic symmetry, with dihedral group of order : they are unchanged when rotated of a turn around the axis of symmetry, reflected across any plane passing through both apices and a base vertex or both apices and the center of a base edge, or reflected across the mirror plane. Because their faces are transitive under these symmetry transformations, they are Isohedral figure. They are the dual polyhedron of prisms and the prisms are the dual of bipyramids as well; the bipyramids vertices correspond to the faces of the prism, and the edges between pairs of vertices of one correspond to the edges between pairs of faces of the other, and vice versa. The prisms share the same symmetry as the bipyramids. The regular octahedron is more symmetric still, as its base vertices and apices are indistinguishable and can be exchanged by reflections or rotations; the regular octahedron and its dual, the cube, have octahedral symmetry.

The volume of a symmetric bipyramid is $$\backslash frac\{2\}\{3\}Bh,$$ where is the area of the base and the perpendicular distance from the base plane to either apex. In the case of a regular sided polygon with side length and whose altitude is , the volume of such a bipyramid is: $$\backslash frac\{n\}\{6\}hs^2\; \backslash cot\; \backslash frac\{\backslash pi\}\{n\}.$$

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Related and other types of bipyramid

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Concave bipyramids A concave bipyramid has a concave polygon base, and one example is a concave tetragonal bipyramid or an irregular concave octahedron. A bipyramid with an arbitrary polygonal base could be considered a right bipyramid if the apices are on a line perpendicular to the base passing through the base's centroid.

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Asymmetric bipyramids An asymmetric bipyramid has apices which are not mirrored across the base plane; for a right bipyramid this only happens if each apex is a different distance from the base.

The Dual polyhedron of an asymmetric right -gonal bipyramid is an -gonal frustum.

A regular asymmetric right -gonal bipyramid has symmetry group , of order .

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Scalene triangle bipyramids An isotoxal right (symmetric) di--gonal bipyramid is a right (symmetric) -gonal bipyramid with an Isotoxal figure flat polygon base: its basal vertices are coplanar, but alternate in two Radius.

All its faces are congruent , and it is Isohedral figure. It can be seen as another type of a right symmetric di--gonal scalenohedron, with an isotoxal flat polygon base.

An isotoxal right (symmetric) di--gonal bipyramid has two-fold rotation axes through opposite basal vertices, reflection planes through opposite apical edges, an -fold rotation axis through apices, a reflection plane through base, and an -fold rotation-reflection axis through apices, representing symmetry group of order . (The reflection about the base plane corresponds to the rotation-reflection. If is even, then there is an inversion symmetry about the center, corresponding to the rotation-reflection.)

Example with :

An isotoxal right (symmetric) ditrigonal bipyramid has three similar vertical planes of symmetry, intersecting in a (vertical) -fold rotation axis; perpendicular to them is a fourth plane of symmetry (horizontal); at the intersection of the three vertical planes with the horizontal plane are three similar (horizontal) -fold rotation axes; there is no center of inversion symmetry, but there is a center of symmetry: the intersection point of the four axes.

Example with :

An isotoxal right (symmetric) ditetragonal bipyramid has four vertical planes of symmetry of two kinds, intersecting in a (vertical) -fold rotation axis; perpendicular to them is a fifth plane of symmetry (horizontal); at the intersection of the four vertical planes with the horizontal plane are four (horizontal) -fold rotation axes of two kinds, each perpendicular to a plane of symmetry; two vertical planes bisect the angles between two horizontal axes; and there is a centre of inversion symmetry.

Double example:

• The bipyramid with isotoxal -gon base vertices and right symmetric apices $$\backslash begin\{alignat\}\{5\}$$

 U &= (1,0,0), & \quad V &= (0,2,0), & \quad A &= (0,0,1), \\
 U' &= (-1,0,0), & \quad V' &= (0,-2,0), & \quad A' &= (0,0,-1),
     

\end{alignat} has its faces isosceles. Indeed:

• Upper apical edge lengths:$$\backslash begin\{align\}$$

 \overline{AU} &= \overline{AU'} = \sqrt{2} \,, \\[2pt]
 \overline{AV} &= \overline{AV'} = \sqrt{5} \,;
     

\end{align}

• Base edge lengths: $$$$

 \overline{UV} = \overline{VU'} = \overline{U'V'} = \overline{V'U} = \sqrt{5} \,;
     

• Lower apical edge lengths (equal to upper edge lengths):$$\backslash begin\{align\}$$

 \overline{A'U} &= \overline{A'U'} = \sqrt{2} \,, \\[2pt]
 \overline{A'V} &= \overline{A'V'} = \sqrt{5} \,.
     

\end{align}

• The bipyramid with same base vertices, but with right symmetric apices $$\backslash begin\{align\}$$

 A &= (0,0,2), \\
 A' &= (0,0,-2),
     

\end{align} also has its faces isosceles. Indeed:

• Upper apical edge lengths:$$\backslash begin\{align\}$$

 \overline{AU} &= \overline{AU'} = \sqrt{5} \,, \\[2pt]
 \overline{AV} &= \overline{AV'} = 2\sqrt{2} \,;
     

\end{align}

• Base edge length (equal to previous example): $$$$

 \overline{UV} = \overline{VU'} = \overline{U'V'} = \overline{V'U} = \sqrt{5}\,;
     

• Lower apical edge lengths (equal to upper edge lengths):$$\backslash begin\{align\}$$

 \overline{A'U} &= \overline{A'U'} = \sqrt{5}\,, \\[2pt]
 \overline{A'V} &= \overline{A'V'} = 2\sqrt{2}\,.
     

\end{align}

In crystallography, isotoxal right (symmetric) didigonal (8-faced), ditrigonal (12-faced), ditetragonal (16-faced), and dihexagonal (24-faced) bipyramids exist.

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Scalenohedra A scalenohedron is similar to a bipyramid; the difference is that the scalenohedra has a zig-zag pattern in the middle edges.

It has two apices and basal vertices, faces, and edges; it is topologically identical to a -gonal bipyramid, but its basal vertices alternate in two rings above and below the center.

All its faces are congruent , and it is Isohedral figure. It can be seen as another type of a right symmetric di--gonal bipyramid, with a regular zigzag skew polygon base.

A regular right symmetric di--gonal scalenohedron has two-fold rotation axes through opposite basal mid-edges, reflection planes through opposite apical edges, an -fold rotation axis through apices, and a -fold rotation-reflection axis through apices (about which rotations-reflections globally preserve the solid), representing symmetry group of order . (If is odd, then there is an inversion symmetry about the center, corresponding to the rotation-reflection.)

Example with :

A regular right symmetric ditrigonal scalenohedron has three similar vertical planes of symmetry inclined to one another at and intersecting in a (vertical) -fold rotation axis, three similar horizontal -fold rotation axes, each perpendicular to a plane of symmetry, a center of inversion symmetry, and a vertical -fold rotation-reflection axis.

Example with :

A regular right symmetric didigonal scalenohedron has only one vertical and two horizontal -fold rotation axes, two vertical planes of symmetry, which bisect the angles between the horizontal pair of axes, and a vertical -fold rotation-reflection axis; it has no center of inversion symmetry.

For at most two particular values of $z\_A\; =\; |z\_\{A\text{'}\}|,$ the faces of such a scalenohedron may be isosceles.

Double example:

• The scalenohedron with regular zigzag skew -gon base vertices and right symmetric apices $$\backslash begin\{alignat\}\{5\}$$

 U &= (3,0,2), & \quad V &= (0,3,-2), & \quad A &= (0,0,3), \\
 U' &= (-3,0,2), & \quad V' &= (0,-3,-2), & \quad A' &= (0,0,-3),
     

\end{alignat} has its faces isosceles. Indeed:

• Upper apical edge lengths:$$\backslash begin\{align\}$$

 \overline{AU} &= \overline{AU'} = \sqrt{10} \,, \\[2pt]
 \overline{AV} &= \overline{AV'} = \sqrt{34} \,;
     

\end{align}

• Base edge length:$$$$

 \overline{UV} = \overline{VU'} = \overline{U'V'} = \overline{V'U} = \sqrt{34} \,;
     

• Lower apical edge lengths (equal to upper edge lengths swapped):$$\backslash begin\{align\}$$

 \overline{A'U} &= \overline{A'U'} = \sqrt{34} \,, \\[2pt]
 \overline{A'V} &= \overline{A'V'} = \sqrt{10} \,.
     

\end{align}

• The scalenohedron with same base vertices, but with right symmetric apices$$\backslash begin\{align\}$$

 A &= (0,0,7), \\
 A' &= (0,0,-7),
     

\end{align} also has its faces isosceles. Indeed:

• Upper apical edge lengths:$$\backslash begin\{align\}$$

 \overline{AU} &= \overline{AU'} = \sqrt{34} \,, \\[2pt]
 \overline{AV} &= \overline{AV'} = 3\sqrt{10} \,;
     

\end{align}

• Base edge length (equal to previous example): $$$$

 \overline{UV} = \overline{VU'} = \overline{U'V'} = \overline{V'U} = \sqrt{34} \,;
     

• Lower apical edge lengths (equal to upper edge lengths swapped):$$\backslash begin\{align\}$$

 \overline{A'U} &= \overline{A'U'} = 3\sqrt{10} \,, \\[2pt]
 \overline{A'V} &= \overline{A'V'} = \sqrt{34} \,.
     

\end{align}

In crystallography, regular right symmetric didigonal (-faced) and ditrigonal (-faced) scalenohedra exist.

The smallest geometric scalenohedra have eight faces, and are topologically identical to the regular octahedron. In this case (), in crystallography, a regular right symmetric didigonal (-faced) scalenohedron is called a tetragonal scalenohedron.

Let us temporarily focus on the regular right symmetric -faced scalenohedra with i.e. $$$$

 z_{A} = |z_{A'}| = x_{U} = |x_{U'}| = y_{V} = |y_{V'}|.
     

Their two apices can be represented as and their four basal vertices as : $$\backslash begin\{alignat\}\{5\}$$

 U &= (1,0,z), & \quad V &= (0,1,-z), & \quad A &= (0,0,1), \\
 U' &= (-1,0,z), & \quad V' &= (0,-1,-z), & \quad A' &= (0,0,-1),
     

\end{alignat} where is a parameter between and .

At , it is a regular octahedron; at , it has four pairs of coplanar faces, and merging these into four congruent isosceles triangles makes it a disphenoid; for , it is concave.

Example: geometric variations with regular right symmetric 8-faced scalenohedra: ! ! ! ! !

If the -gon base is both Isotoxal figure in-out and Skew polygon, then not all faces of the isotoxal right symmetric scalenohedron are congruent.

Example with five different edge lengths:

• The scalenohedron with isotoxal in-out zigzag skew -gon base vertices and right symmetric apices $$\backslash begin\{alignat\}\{5\}$$

 U &= (1,0,1), & \quad V &= (0,2,-1), & \quad A &= (0,0,3), \\
 U' &= (-1,0,1), & \quad V' &= (0,-2,-1), & \quad A' &= (0,0,-3),
     

\end{alignat} has congruent scalene upper faces, and congruent scalene lower faces, but not all its faces are congruent. Indeed:

• Upper apical edge lengths:$$\backslash begin\{align\}$$

 \overline{AU} &= \overline{AU'} = \sqrt{5} \,, \\[2pt]
 \overline{AV} &= \overline{AV'} = 2\sqrt{5} \,;
     

\end{align}

• Base edge length:$$$$

 \overline{UV} = \overline{VU'} = \overline{U'V'} = \overline{V'U} = 3;
     

• Lower apical edge lengths:$$\backslash begin\{align\}$$

 \overline{A'U} &= \overline{A'U'} = \sqrt{17} \,, \\[2pt]
 \overline{A'V} &= \overline{A'V'} = 2\sqrt{2} \,.
     

\end{align}

For some particular values of , half the faces of such a scalenohedron may be isosceles or equilateral.

Example with three different edge lengths:

• The scalenohedron with isotoxal in-out zigzag skew -gon base vertices and right symmetric apices $$\backslash begin\{alignat\}\{5\}$$

 U &= (3,0,2), & \quad V &= \left( 0,\sqrt{65},-2 \right), & \quad A &= (0,0,7), \\
 U' &= (-3,0,2), & \quad V' &= \left( 0,-\sqrt{65},-2 \right), & \quad A' &= (0,0,-7),
     

\end{alignat} has congruent scalene upper faces, and congruent equilateral lower faces; thus not all its faces are congruent. Indeed:

• Upper apical edge lengths:$$\backslash begin\{align\}$$

 \overline{AU} &= \overline{AU'} = \sqrt{34} \,, \\[2pt]
 \overline{AV} &= \overline{AV'} = \sqrt{146} \,;
     

\end{align}

• Base edge length:$$$$

 \overline{UV} = \overline{VU'} = \overline{U'V'} = \overline{V'U} = 3\sqrt{10} \,;
     

• Lower apical edge length(s): $$\backslash begin\{align\}$$

 \overline{A'U} &= \overline{A'U'} = 3\sqrt{10} \,, \\[2pt]
 \overline{A'V} &= \overline{A'V'} = 3\sqrt{10} \,.
     

\end{align}

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Star bipyramids A star bipyramid has a star polygon base, and is self-intersecting.

A regular right symmetric star bipyramid has congruent isosceles triangle faces, and is Isohedral figure.

A -bipyramid has Coxeter diagram .

Example star bipyramids:

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4-polytopes with bipyramidal cells The dual of the rectification of each convex regular 4-polytopes is a cell-transitive 4-polytope with bipyramidal cells. In the following:

• is the apex vertex of the bipyramid;
• is an equator vertex;
• is the distance between adjacent vertices on the equator (equal to 1);
• is the apex-to-equator edge length;
• is the distance between the apices.

The bipyramid 4-polytope will have vertices where the apices of bipyramids meet. It will have vertices where the type vertices of bipyramids meet.

• bipyramids meet along each type edge.
• bipyramids meet along each type edge.
• is the cosine of the dihedral angle along an edge.
• is the cosine of the dihedral angle along an edge.

As cells must fit around an edge, $$\backslash begin\{align\}$$

 N_\overline{EE} \arccos C_\overline{EE} &\le 2\pi, \\[4pt]
 N_\overline{AE} \arccos C_\overline{AE} &\le 2\pi.
     

\end{align}

4-polytopes with bipyramidal cells !colspan=9	4-polytope properties !colspan=6	Bipyramid properties
R. 5-cell		10	5	5	4	6	3	3	Triangular		$\backslash frac23$	0.667	$-\backslash frac17$	$-\backslash frac17$
R. tesseract		32	16	8	4	12	3	4	Triangular		$\backslash frac\{\backslash sqrt\{2\}\}\{3\}$	0.624	$-\backslash frac25$	$-\backslash frac15$
R. 24-cell		96	24	24	8	12	4	3	Triangular		$\backslash frac\{2\; \backslash sqrt\{2\}\}\{3\}$	0.745	$\backslash frac1\{11\}$	$-\backslash frac5\{11\}$
R. 120-cell		1200	600	120	4	30	3	5	Triangular		$\backslash frac\{\backslash sqrt\{5\}\; -\; 1\}\{3\}$	0.613	$-\; \backslash frac\{10\; +\; 9\backslash sqrt\{5\}\}\{61\}$	$-\; \backslash frac\{7\; -\; 12\backslash sqrt\{5\}\}\{61\}$
R. 16-cell		24	8	16	6	6	3	3	Square bipyramid		$\backslash sqrt\{2\}$	1	$-\backslash frac13$	$-\backslash frac13$
R. cubic honeycomb		∞	∞	∞	6	12	3	4	Square bipyramid		$1$	0.866	$-\backslash frac12$	$0$
R. 600-cell		720	120	600	12	6	3	3	Pentagonal		$\backslash frac\{5\; +\; 3\backslash sqrt\{5\}\}\{5\}$	1.447	$-\; \backslash frac\{11\; +\; 4\backslash sqrt\{5\}\}\{41\}$	$-\; \backslash frac\{11\; +\; 4\backslash sqrt\{5\}\}\{41\}$

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Other dimensions A generalized -dimensional "bipyramid" is any -polytope constructed from an -polytope base lying in a hyperplane, with every base vertex connected by an edge to two apex vertices. If the -polytope is a regular polytope and the apices are equidistant from its center along the line perpendicular to the base hyperplane, it will have identical pyramidal facets.

A 2-dimensional analog of a right symmetric bipyramid is formed by joining two congruent isosceles triangles base-to-base to form a rhombus. More generally, a kite is a 2-dimensional analog of a (possibly asymmetric) right bipyramid, and any quadrilateral is a 2-dimensional analog of a general bipyramid.

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See also

• Trapezohedron

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Notes

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Citations

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Works cited

• Anthony Pugh (1976). 9780520030565, University of California Press Berkeley. ISBN 9780520030565
  Chapter 4: Duals of the Archimedean polyhedra, prisms and antiprisms

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External links

• The Uniform Polyhedra
• Virtual Reality Polyhedra The Encyclopedia of Polyhedra
• VRML models (George Hart) <3> <4> <5> <6> <7> <8> <9> <10>
• Conway Notation for Polyhedra Try: "dP n", where n = 3, 4, 5, 6, ... Example: "dP4" is an octahedron.

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