Earth Materials. John O'Brien

symmetries.

Only 32 different three‐dimensional motif symmetries exist. These define 32 space point groups, each with unique space point group symmetry. In minerals, the 32 crystal classes – to one of which all minerals belong – correspond to the 32 space point group symmetries of the mineral's three‐dimensional motif. That the crystal classes were originally defined on the basis of the external symmetry of mineral crystals is another example of the fact that the external symmetry of minerals reflects the internal symmetry of their constituents. The 32 crystal classes belong to 6 (or 7) crystal systems, each with its own characteristic symmetry. Table 4.3 summarizes the crystal systems, the symmetries of the 32 space point groups or crystal classes and their names, which are based on general crystal forms. It is important to remember that a crystal cannot possess more symmetry than that of the motifs of which it is composed. However, it can possess less, depending on how the motifs are arranged and how the crystal developed during growth.

      4.4.2 Bravais lattices, unit cells, and crystal systems

      As noted earlier, any motif can be represented by a point called a node. Nodes, and the motifs they represent, can also be translated in three directions (t_a, t_b, and t_c) to produce three‐dimensional space point lattices and unit cells (Figure 4.10).

      Unit cells are the three‐dimensional analogs of unit meshes. A unit cell is a parallelepiped whose edge lengths and volume are defined by the three unit translation vectors (t_a, t_b, and t_c). The unit cell is the smallest unit that contains all the information necessary to reproduce the mineral by three‐dimensional symmetry operations. Unit cells may be primitive (P), in which case they have nodes only at their corners and a total content of one node (=one motif). Non‐primitive cells are multiple because they contain extra nodes in one or more faces (A, B, C or F) or in their centers (I) and possess a total unit cell content of more than one node or motif.

Unit cells bear a systematic relationship to the coordination polyhedra and packing of atoms that characterize mineral structures, as illustrated by Figure 4.11.

In 1850, Bravais recognized that only 14 basic types of three‐dimensional translational point lattices exist; these are known as the 14 Bravais space point lattices (Klein and Hurlbut 1985) and define 14 basic types of unit cells. The 14 Bravais lattices are distinguished on the basis of (1) the magnitudes of the three unit translation vectors t_a, t_b, and t_c or more simply a, b, and c, (2) the angles (alpha, beta, and gamma) between them, where (α = b Λ c; β = c Λ a; γ = a Λ b), and (3) whether they are primitive lattices or some type of multiple lattice. Figure 4.12 illustrates the 14 Bravais space point lattices.

The translational symmetry of every mineral can be represented by one of the 14 basic types of unit cells. Each unit cell contains one or more nodes that represent motifs and contains all the information necessary to characterize chemical composition. Each unit cell also contains the rules according to which motifs are repeated by translation; the repeat distances, given by t_a = a, t_b = b, t_c = c, and directions, given by angles α, β, and γ. The 14 Bravais lattices can be grouped into crystal systems on the basis of the relative dimensions of the unit cell edges (a, b, and c) and the angles between them (α, β, and γ). These six (or seven if the hexagonal system is divided into trigonal and hexagonal) systems in which all minerals crystallize. These include the isometric (cubic), tetragonal, orthorhombic, monoclinic, triclinic, and hexagonal systems. The latter is subdivided into the hexagonal division or system and the trigonal (rhombohedral) division or system. Table 4.4 summarizes the characteristics of the Bravais lattices in the major crystal systems.

Table 4.3 The six crystal systems and 32 crystal classes, with their characteristic symmetry and crystal forms.

System	Crystal class	Class symmetry	Total symmetry
Isometric	Hexoctahedral		3A4, , 6A2, 9m
	Hextetrahedral		, 4A3, 6m
	Gyroidal	432	3A4, 4A3, 6A2
	Diploidal		3A2, 3m,
	Tetaroidal	23	3A2, 4A3
Tetragonal	Ditetragonal–dipyramidal	4/m2/m2/m	i, 1A4, 4A2, 5m
	Tetragonal–scalenohedral		, 2A2, 2m
	Ditetragonal–pyramidal	4mm	1A4, 4m
	Tetragonal–trapezohedral	422	1A4, 4A2
	Tetragonal–dipyramidal	4/m	i, 1A4, 1m
	Tetragonal–disphenoidal
	Tetragonal–pyramidal	4	1A4
Hexagonal(hexagonal)