Morphology — where it appears
Named by 4 essays across one field — each of them below, with the objects they name alongside it.
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.
The fast faces are the ones that vanish
A crystal has two predicted shapes and they are not the same. One minimises surface energy and is what a crystal settles into; the other is what growth leaves behind, and in it a face that grows quickly grows itself out of existence.
A zone is a vanishing dot product
Look at a crystal and the obvious thing about it is that the faces run in bands — sets whose edges are all parallel. A face belongs to such a band exactly when three integers multiplied by three others sum to zero. No length enters, no angle enters, and that is why every index on a nineteenth-century mineral specimen is still the index used now.
Which faces are flat
Bravais ranks a crystal's faces by how far apart their planes lie. Hartman and Perdok classify them by how many uninterrupted chains of bonds run inside them, which uses no spacing at all — and on the three cubic structures the two rules put the same face first every time. Then the second rule's power turns out to live entirely in where the chain list is cut off.
Named alongside it
The objects these essays reach for when they reach for this one.
Crystal formBfdhCrystal habitInterplanar spacingMiller indicesMeasurementSystematic absenceBroken-bondCentringClose packingCoordination numberCrystal net