The angles between the faces of {102̅}
The form {102̅} of class 3̅m in section, with each face labelled by its indices. Its 6 faces make 15 pairs and only 3 distinct angles, the smallest being 76.43°. Every value is computed from the cell's metric — the one calculation in this family that is not integer arithmetic, because an angle is a real number and a lattice does not constrain it.
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Where it is called
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Symmetry at work
Why a crystal face carries small whole numbers
A crystal face is flat because it lies on a plane of lattice points, and its orientation is therefore named by three integers rather than by two angles. That the integers exist is a theorem about lattices; that they are usually smaller than four is a separate claim about growth, and the two are routinely run together.
Symmetry at work
The angles belong to the substance, the shape to the specimen
Two crystals of the same mineral can look nothing like each other and still have exactly the same angles between corresponding faces. That is the oldest quantitative law in the subject, and what it measures turns out to be the shape of the unit cell — which means a brass instrument from 1809 was reading lattice parameters a century before anyone knew there were any.
Symmetry at work
Which faces a crystal shows
Rock salt grows as cubes, fluorite as octahedra, garnet as dodecahedra. All three have cubic lattices and the same list of possible faces, and what separates them is which reflections are systematically absent — a rule about diffraction predicting a shape a mineralogist can hold.