Details

In general, the two complementary blocks take the shape of a concave and a convex pentagonal dodecahedron, respectively. Both exhibit the symmetry of a pyritohedron, which is a polyhedron bounded by 12 axially symmetric (but not regular) convex pentagons (the crystal form of the sulfur mineral pyrite). This symmetry is determined by three mutually perpendicular mirror planes and four three-fold rotation axes (the direction of these axes is that of the four body diagonals of the cube). Hence, it is less than the symmetry of the regular pentagonal dodecahedron. However, there is an intermediate stage when the second block takes on just this latter, regular shape. On the other hand, in the extreme case corresponding to the volume ratio 0:1, the symmetry is that of the cube. In this case, the first block degenerates to a quadruple of line segments passing through a common point (in fact, the quadruple of the body diagonals of the cube). The second block, in turn, becomes a rhombic dodecahedron congruent to the starting figure. Thus, one sees how a rhombic dodecahedron can be decomposed into six equal tetragonal bipyramids with a common apex; then, after a half-turn of each, they reassemble to form another rhombic dodecahedron ("turning the rhombic dodecahedron inside out").

The continuous change of the shape of the two blocks described above is illustrated by a nice series of figures in [1].

Our Demonstration can be considered as another illustration of the transformation of polyhedral shapes described by Branko Grünbaum.

Reference

[1] B. Grünbaum, "Acoptic Polyhedra," in Advances in Discrete and Computational Geometry: Proceedings of the 1996 AMS-IMS-SIAM Joint Summer Research Conference, South Hadley, MA (B. Chazelle, J. E. Goodman, and R. Pollack, eds.), Providence, RI: American Mathematical Society, 1996 pp. 163–199.