The  Rhombic  Triacontahedron

 

 

The Rhombic Triacontahedron is an extremely fascinating polyhedron. It is built around the dodecahedron, and like the dodecahedron, it has many phi relationships within it. This polyhedron contains all five of the Platonic Solids directly on its vertices, and shows the proper relationship between them.
The  Rhombic Triacontahedron (hereinafter referred to as r.t.) has 30 faces, 60 edges, and 32 vertices.

Figure 1 -- showing the front portion of the Rhombic Triacontahedron (red) with
the sides of the dodecahedron (gray)

Notice  pentagon CDNJO, then notice Z. Z is raised off the pentagon (a distance we shall find later on) and Z is connected to all 5 vertices of the pentagonal face of the dodecahedron. This can be seen even more clearly at U. The pentagon GPIJO has all of its vertices connected to U. Of course, we could have drawn this figure without the dodecahedron faces, which is obviously not part of the r.t., but it helps for clarity.
Notice that the faces of the r.t. are diamond-shaped, somewhat like the rhombic dodecahedron, but these faces are longer and skinnier. Look at the r.t. face UOZJ at the upper left.  U and Z are the long-axis vertices. Notice that the line between O and J, the short-axis vertices, form one of the edges (sides) of the dodecahedron.
The dual of the r.t. is the icosa-dodecahedron.
The r.t. is more clearly spherical than any of the polyhedra we have studied so far.

Notice also: In Figure 2 below, we see that the rhombic triacontahedron has internal pentagonal planes just like the icosahedron and the dodecahedron!

Figure 2 -- showing the internal pentagonal planes of the r.t. Figure 2 is rotated 180 degrees with respect to Figure 1.

Note the large  highlighted pentagons. The lengths of all of the large internal pentagon sides are precisely the long axis of every r.t. face! For example, look at VZ and ZFo in the top pentagonal plane and EoBo in the lower pentagonal plane.
 
The r.t. has a circumsphere and an inner sphere. The circumsphere goes around all 20 of the vertices that rise off the faces of the dodecahedron.
The diameter of the circumsphere is UW. UW is in green in Figure 2. O' is the centroid.  The circumsphere touches all of the vertices that are raised off the pentagonal planes of the dodecahedron. There are 12 of these, because there are 12 faces on the dodecahedron.
The inner sphere touches all of the 20 vertices of the dodecahedron. The diameter of the inner sphere would be, for example, IL. UW > IL.
This leads us to think that possibly, the relationship between U, Go,O',Ho and W will be similar to those of  the dodecahedron and the icosahedron. Later on, we will see that this is indeed the case.
 

Notice also that the rhombic triacontahedron inherently contains within it not only a dodecahedron, but an icosahedron as well! Notice that the 12 vertices which rise off the dodecahedron faces provide the 12 vertices of the icosahedron.  Remember that the dual of the dodecahedron is the icosahedron and that the dual is formed by taking points at the center of the faces.

Figure 3 -- showing the 12 vertices of the icosahedron (blue) within the rhombic triacontahedron

The sides of the icosahedron are the long axes of the r.t. faces.
The sides of the dodecahedron are the short axes of the r.t. faces.
Therefore the rhombic triacontahedron is just the combination of the dodecahedron with its dual, the icosahedron.
The rhombic triacontahedron  is the model nature uses to demonstrate the true relationship between the side of the icosahedron and the side of the dodecahedron. We will see later on that these relationships are based on .

Note also that when a cube is inscribed within 8 of the 12 vertices belonging to the dodecahedron within the rhombic triacontahedron, the lengths of the cube sides are precisely equal to the long axis of any of the rhombic triacontahedron rhombi. Furthermore, the sides of the cube are precisely equal to any of the diagonals of the pentagonal faces of the dodecahedron:

Figure 3A
The sides of the cube, in blue, are also the diagonals of the pentagonal faces of the dodecahedron within the rhombic triacontahedron.


Since the tetrahedron (one tetrahedron in green, the other in purple) and the octahedron (in orange) can be inscribed within the cube, the rhombic triacontahedron shows the precise relationship between the Platonic Solids!


Figure 3B -- The cube, 2 interlocking tetrahedrons, and the octahedron inside a cube

The Rhombic Triacontahedron therefore elegantly describes the nesting of the five Platonic Solids:  icosahedron, dodecahedron, cube, tetrahedron, octahedron. When the sides of the octahedron are divided in Mean and Extereme (Phi) Ratio, another icosahedron is formed. This begins the process all over again, and shows that the 5 nested Platonic Solids may not only grow and contract to infinity, but do so in a perfectly harmonious way.

Figure 3B -- Showing how the icosahedron nests  within the octahedron. Interestingly, the icosahedron is formed within the octahedron by dividing each edge of the octahedron in Phi Ratio.

 

What is the volume of the rhombic triacontahedron?
As before we use the pyramid method. There are 30 faces, so there are 30 pyramids. Imagine a point at the very center of the r.t. If you connect that point up with one of the faces, you will have a pyramid that looks like this:

Figure 4 -- one of the 30 pyramids of the rhombic triacontahedron. O'Z is the height of
the pyramid. O'U = O'V = radius of outer sphere which touches the 12 r.t. vertices which are raised off the center of the dodecahedron face. O'I = O'J = radius of inner sphere which touches all 20 of the short-axis r.t. vertices, which are also the vertices of the dodecahedron

We want to find the volume of the r.t. in terms of the r.t. side. However, we don't know the length of the r.t side! But we do  know the length of the side of the dodecahedron, in terms of a unit sphere which touches all the vertices of the dodecahedron. So let's try to get the r.t. side (hereinafter referred to as rts) in terms of the dodecahedron side.

Figure 5                   Figure 5A

Figure 5 and 5A show the following important data:
V is one of the 12 raised vertices of the r.t. off the face of the dodecahedron.
C is the center of the dodecahedron face. C lies in the plane of IJOGP, and is directly below V.
Z is the center of the r.t. face IUJV (see Figure 4), and also the mid-edge of the side of the dodec.
IVJ (in red) is  one-half of the r.t. diamond face IUJV (see Figure 4)
O'Z is the distance from centroid to mid-edge of the dodec face. This is the height of the r.t. pyramid.
ZV is the distance from mid-edge of dodecahedron to the raised vertex V off the dodecahedron face.
ZC is the distance from mid-edge of dodecahedron to center of dodecahedron face.
CV is the distance of V off the center of the dodecahedron face.
Figure 5A shows that O'CV is a straight line, so that ZO'C = ZO'V.
O'ZV is right.
O'CZ is right.

From this data we can show that the triangles O'ZV, O'CZ, and CZV are similar by  angle-side-angle.
First we show the triangle O'ZV and O'CZ are similar:
O'ZV is right, so is O'CZ.
O'Z is common to both triangles.
ZO'V = ZO'C.     Therefore both triangles are similar by ASA.

Now we show that triangle CZV is similar to triangle O'ZV by angle-side-angle.
ZCV and O'ZV are right.
ZV is common to both triangles.
O'VZ = CVZ.  
Therefore both triangles are similar by angle-side-angle.

With this information we can determine CV, the distance of the vertex V off of the dodec face, and ZV, which will enable us to get the side of the r.t. in terms of the side of the dodecahedron.

Since all 3 triangles are similar, we can write the following relationship:
CZ / O'C = CV / CZ.
The distances  O'Z, O'C, and CZ are known. From  Dodecahedron it is known that
   (ds means  dodecahedron side)
 
 

 
 
Now we have CV, the distance from the plane of the dodecahedron to the rhombic triacontahedron “cap” over the dodecahedron face, in terms of the dodecahedron side.

Now we need to find ZV, so that we can get IV, the length of the side or edge of the rhombic triacontahedron. We can write the following relationship:

Refer back to Figures 4 and 5. Now that we have ZV, we can find the side of the r.t., IV.
The triangle IVJ in Figure 4 and 5 is one-half of an r.t face. We have already calculated ZV, and we know that IZ is just one–half the side of the side of the dodecahedron, ds. We also know that the angle IZV is right by construction. 
Therefore,  by the Pythagorean Theorem,
 

Here we have established an important fact: we have related the side of the rhombic triacontahedron, or rts, to the side of the dodecahedron and, therefore, to the radius of the unit sphere which encloses all 20 vertices of the dodecahedron and, in turn, the short axis vertices of the rhombic triacontahedron.

We can now describe the distance of any vertex of the r.t. off the plane of  the dodecahedron, CV, in terms of the side of the r.t. We may now write

Let's now find the radius of the outer sphere of the r.t. in terms of the side of the r.t. itself. Remember that the outer sphere touches all 12 long-axis vertices of the r.t., and that these 12 vertices are the vertices of an icosahedron

We need to convert these distances so that they are related to rts, not ds.
 

In the Rhombic Triacontahedron, the relationship between the side and the radius of the enclosing sphere is Phi.

What is ? This is just the unit sphere which touches all 20 vertices of the dodecahedron. We know from  Dodecahedron  that
Converting this to the side of the r.t. we have:
 

Now we have enough information to calculate the volume of the rhombic triacontahedron in terms of it's own side. Refer back to Figures 4 and 5 for diagrams.
We can calculate the area of the r.t. face, because we know IJ and ZV, which we can use to give us the area of one-half the face of the r.t. We see from Figure 4 that O’Z, the height of the r.t. pyramid, is just the distance from the centroid to the mid-edge of any of the sides of the dodecahedron. We know from Dodecahedron, that this distance is. We have to do some conversions of these values first, to get them all in terms of the rts.

To get the area of the r.t. face, divide it into 2 identical triangles at the short axis IJ, find the area of one triangle, and multiply by 2..
The area of any triangle is 1/2 * base * height, so the area of the r.t. face is twice this value.
IJ is just the side of the dodecahedron, and it is the base of our triangle.
 
There are 30 pyramids for 30 faces so total volume  is:
 

The volume of the r.t. can be calculated another way. Since the r.t. is built upon the dodecahedron, the r.t. volume is just the volume of the dodecahedron + the extra volume of all of the little 12 pentagonal pyramids formed from the raised vertices off the 12 pentagonal faces of the dodecahedron. To see this, check Figure 1 again and look at U-IJOGP or V- IJNFM.
The volume of the dodecahedron is, from  Dodecahedron ,
 
Converting this to the side of the r.t. we get:
 

The volume of each of the 12 "extra" pyramids =
   1/3 * area of pentagon * CV (height of each raised vertex off of the face of the dodecahedron) =
 
We only have one problem: one of our values is in terms of the dodecahedron side. We need to convert that to the side of the r.t.
 

What is the surface area of the rhombic triacontahedron?

Before we calculate the central and surface angles of the rhombic triacontahedron, let us complete our research into the distances from the centroid to various points of interest on this polyhedron.
We have already calculated the distances to the small and large axis vertices, and to the mid-face. Now we need to find the distance from the centroid to any mid-edge.


Figure 4a
Showing the right triangle O’ZA’
We are looking for OA’. We may write
. We know O’Z, but what is ZA’?
IZ = ½ IJ by construction.
JA’ = ½ JV by construction.
The triangles VIJ and ZA’J are congruent by angle-angle-angle. Triangle VIJ is isosceles by construction, therefore triangle ZA’J is isosceles and ZA’ = ½rts.


What are the central angles of the rhombic triacontahedron?


Figure 4, repeated
There are 3 central angles of the r.t. that are of interest. Refer to Figure 4.
The first is UO'V, central angle of the long-axis
The second is IO'J, central angle of the short-axis.
The third and primary central angle is IO'V, the central angle of each adjacent side.

O'Z is perpendicular to IJ, and to the plane of the r.t. face, IUJV.
O'Z bisects IJ at Z.
Triangles UO'Z and VO'Z are right.
So we can write 
 
We recognize this angle (see Phi Ratio Triangle ) as being part of a  ratio triangle.
The ratio's of these distances are shown below in Figure 6:
Figure 6 --- showing the relationship between VZ, O'Z, O'V

Now UO'V = 2 *ZO'V, so
UO'V = 63.4349488°.

Let's find IO'J, the central angle of the small axis of the r.t. face.
IO'Z and ZO'J are right. So we write
 
We know IZ = one half the side of the dodecahedron, or 1/2 * ds.
From above we know that
 
Therefore <IO'J = 2 *IO'Z = 41.81031488°.
Note that IZ / O’Z =, so that IZ and O’Z have a relationship based on the square of .
 
Figure 7  -- showing the relationship between O'Z, IZ and O'I
This division is in ratio  .

To find IO'V, recognize that the point V lies in a straight line directly above the center of the dodecahedron face. So the angle from IO'V  is the same as the angle from I to O' to a point (G) in the middle of the dodecahedron face.

Figure 8 -- showing that the central angle IO'V = the angle IO'G

The triangle O'GI is right by construction, so we need only to know GI and O'G.
We know from   Area of the Pentagon that,
and from  Dodecahedron we know the distance
.

What are the surface angles of the rhombic triacontahedron?
Observe from Figure 4 that the angles we are looking for are IVJ and UIV.
Z is a bisector of IZ so the triangle IVZ is right.
IV = the side of the r.t. = rts.
, which we already found above.
So we can write
.

We recognize immediately, from The Phi Triangle , that this angle indicates a right triangle whose long and short sides are divided in Extreme and Mean Ratio (Phi ratio).
Therefore
And so the ratio between the long axis VU and the short axis IJ (see Figure 4) must also be in Mean and Extreme Ratio.
Therefore VU / IJ  = .
So the face of the rhombic triacontahedron is a  rhombus.

The face angle we want, IVJ, is then twice IVZ.
IVJ = 63.43494882° = short axis face angle.

One-half of the other face angle, ZIV,  is just 90 - IVZ = 58.28252558°.
So UIV = 116.5650512°.

What are the lengths of the long axis VU and the short axis IJ of the r.t. face?
 

As stated above,
 

What is the dihedral angle of the rhombic triacontahedron?
To see this calculation, click on  R.T. Dihedral Angle .
The dihedral angle = 144°.

The distance from the centroid to any of the 12 long-axis vertices above the dodecahedron faces =
Distance from centroid to any of the 20 short-axis vertices = .

We need to go back to Figure 2 now and look at the diameter of the sphere which encloses the 12 long-axis vertices of the icosahedron. This line is shown in Figure 2 as UO'W. The diameter passes through the centroid at O' and also through the middle of the 2 large pentagonal planes marked in Figure 2.
It also passes through the top and bottom faces of the dodecahedron. These faces are also marked in Figure 2.
There are 4  highlighted pentagonal planes along the diameter UW, as well as the midpoint O'.


Figure 2, repeated
We have the extra distance off the top plane of the dodecahedron to the vertex U, marked as IoU, and the extra distance off the bottom plane of the dodecahedron to the vertex W, marked as JoW.
What are the relationships between U, Io, Go, O', Ho, Jo, and W?
In Figures 5 and 5A, we found the distance off the plane of the dodecahedron face (IoU , JoW ) to be CV. 
CV we found to be  
So IoU = JoW =

Refer back to Figure 2.
Let's find the distance UGo, or the distance from U to the first large pentagonal plane VYCoFoZ.
This will be easy, because we know that the sides of this pentagonal plane are just the long axes of the r.t. We can form a right triangle from U to any one of the vertices of VYCoFoZ, to the center Go. Let's take the right triangle UGoZ. From  Construction of the Pentagon we can get GoZ, it is just the distance from pentagon center to one of the vertices. Inspection of Figure 2 shows that UZ is just the long axis of the r.t. face  UJZO.

Figure 9 -- showing the large internal pentagon VYCoFoZ and the right triangle UGoZ.
Go is the center of the large internal pentagon. U is directly above Go.
The sides of the large pentagon (in green) are all long axes of the r.t. faces, indicated in red.

Triangle UGoZ is right by construction.
 or long-axis of r.t. face.
 
Now we can find  UGo:
 

So UGo = 2 *  UIo and the plane VYCoFoZ of the dodecahedron is twice the distance from U as is the large internal pentagonal plane IPGOJ.
That means UIo = IoGo = 1/2 UGo =  
What is the distance between the centroid O' and the plane IPGOJ, or O'Go?
It is  O'U - UGo.
We know O'U, it is the radius of the outer sphere, or
Therefore,

Now we have enough information to make our distance chart of internal planar distances of the rhombic triacontahedron, just as we did for the icosahedron and the dodecahedron.


Table 1.
Distances between internal planes of the rhombic triacontahedron.
 Table 2. Relationships between distances in Table 1.
(included in the book)

 

From the table of relationships we see that:
O'Io is divided in Extreme and Mean Ratio at Go.
O'Jo is divided in Extreme and Mean Ratio at Ho.
UHo is divided in Mean and Extreme Ratio squared at Go.
WGo is divided in Mean and Extreme Ratio squared at Ho.

Conclusions:
The rhombic triacontahedron  is a combined icosahedron-dodecahedron dual,  so it is not surprising to see so many relationships based on the division in Mean and Extreme Ratio.
The rhombic triacontahedron contains all of the properties of the icosahedron and all of the properties of the dodecahedron and it tells us the proper nesting order of the 5 Platonic Solids. 
 
 


Dihedral Angle Of The Rhombic Triacontahedron



Figure 1.  We are looking for the dihedral angle, BIE . Figure 1 shows an r.t. “cap” (in red) over the face of the dodecahedron, and shows that J and G are on AH, the height of the pentagon. F is directly above the mid-face of the pentagon, at G.  I is directly above J on BE. BJI is right, allowing us to calculate BIJ or EIJ, and BIE, the dihedral angle, is then just twice that.
AH and BE lie on the pentagonal plane ABCDE.
BI is a line along an r.t. face, EI is a line along another of the faces.

Here is our plan of attack:
We know from Rhombic Triacontahedron that BFA is 63.43494882° This can be rewritten without loss of information as . Triangle BIF is right by construction. BF is the side of the r.t., or rts. Here we must use trigonometry to get BI, by taking the sine of BFA so we can find BI. BE is bisected by AH, the angle bisector of BAE and a diagonal of the pentagon.  AJ is known from Pentagon Construction. To get BIJ, we can take the sine of BIJ =  BJ / BI. The dihedral angle BIE is twice angle BIJ.

First let’s find BJ. BJ is one-half the  diagonal of the pentagon with sides equal to the side of the dodecahedron. We must change units in terms of the side of the r.t. Remember that  
So we write  BJ =
= BI / BF.
BI = BF * .
BI =

 

Now we can calculate the dihedral angle BIE.

Figure 4  The dihedral angle BIE
We can write
 
BIJ  = 72°.
The dihedral angle BIE is 2 * BIJ.
Dihedral Angle = 144°.

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