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{{Infobox Polyhedron|
{| border="1" bgcolor="#ffffff" cellpadding="5" align="right" style="margin-left:10px" width="250"
!bgcolor=#e7dcc3 colspan=2|Elongated square gyrobicupola Image_File=elongated square gyrobicupola.png|
Polyhedron_Type=]<br>] -''' J<sub>37</sub>''' - ]|
|-
Face_List=8 ]s<br>18 ]s|
|align=center colspan=2|]
Edge_Count=48|
|-
Vertex_Count=24|
|bgcolor=#e7dcc3|Type||]
Symmetry_Group=''D''<sub>4d</sub>|
|-
Vertex_List=24 of 3.4<sup>3</sup>|
|bgcolor=#e7dcc3|Faces||8 ]s<br>18 ]s
Dual=-|
|-
Property_List=], locally vertex-regular
|bgcolor=#e7dcc3|Edges||48
}}
|-
|bgcolor=#e7dcc3|Vertices||24
|-
|bgcolor=#e7dcc3|Vertex configuration||3.4<sup>3</sup>
|-
|bgcolor=#e7dcc3|]||'']''<sub>4d</sub>
|-
|bgcolor=#e7dcc3|]||-
|-
|bgcolor=#e7dcc3|Properties||convex, locally vertex-regular
|}
In ], the '''elongated square gyrobicupola''' is one of the
]s (''J''<sub>37</sub>). It is locally vertex-regular&mdash;the arrangement of the 4 faces incident on any vertex is the same for all vertices. However, it is not vertex-regular, and consequently not one of the ]s, as the ] of the solid does not act ]ly on the vertices. Basically, two types of vertices can be distinguished by their "neighbours of neighbours". Alternatively, there is exactly one belt of 8 squares around the figure, which distinguishes vertices on the belt from the other vertices.


In ], the '''elongated square gyrobicupola''' is one of the ]s (''J''<sub>37</sub>). As the name suggests, it can be constructed by elongating a ] (''J''<sub>29</sub>) by inserting an ]al ] between its two halves. The resulting solid is locally vertex-regular &mdash; the arrangement of the four faces incident on any vertex is the same for all vertices. However, it is not truly vertex-regular, and consequently not one of the ]s, as the ] of the solid does not act ]ly on the vertices. Essentially, two types of vertices can be distinguished by their "neighbors of neighbors." Another way to see that the polyhedron is not vertex-regular is to note that there is exactly one belt of eight squares around its equator, which distinguishes vertices on the belt from vertices on either side.
It can be constructed by twisting one of the ]e on a ] by 45 degrees. Its similarity to the rhombicuboctahedron gives it the alternative name '''pseudorhombicuboctahedron'''.

The solid can also be seen as the result of twisting one of the ]e (''J''<sub>4</sub>) on a ] (one of the ]s) by 45&nbsp;degrees. Its similarity to the rhombicuboctahedron gives it the alternative name '''pseudorhombicuboctahedron'''.


The 92 Johnson solids were named and described by ] in ]. The 92 Johnson solids were named and described by ] in ].


==External links== ==External link==
* *



Revision as of 04:07, 26 April 2005

Elongated square gyrobicupola
TypeJohnson
J36 - J37 - J38
Faces8 triangles
18 squares
Edges48
Vertices24
Vertex configuration24 of 3.4
Symmetry groupD4d
Dual polyhedron-
Propertiesconvex, locally vertex-regular

In geometry, the elongated square gyrobicupola is one of the Johnson solids (J37). As the name suggests, it can be constructed by elongating a square gyrobicupola (J29) by inserting an octagonal prism between its two halves. The resulting solid is locally vertex-regular — the arrangement of the four faces incident on any vertex is the same for all vertices. However, it is not truly vertex-regular, and consequently not one of the Archimedean solids, as the symmetry group of the solid does not act transitively on the vertices. Essentially, two types of vertices can be distinguished by their "neighbors of neighbors." Another way to see that the polyhedron is not vertex-regular is to note that there is exactly one belt of eight squares around its equator, which distinguishes vertices on the belt from vertices on either side.

The solid can also be seen as the result of twisting one of the square cupolae (J4) on a rhombicuboctahedron (one of the Archimedean solids) by 45 degrees. Its similarity to the rhombicuboctahedron gives it the alternative name pseudorhombicuboctahedron.

The 92 Johnson solids were named and described by Norman Johnson in 1966.

External link

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