Crystal Systems¶
The seven crystal systems and their characteristic symmetry elements.
Interactive Version
For interactive crystal visualizations and detailed data tables, visit gemmology.dev/learn/crystal-systems.
Overview¶
All crystals belong to one of seven crystal systems, classified by their unit cell geometry and symmetry elements. Understanding these systems is fundamental to crystallography and gem identification.
Crystal systems are defined by the relationship between crystallographic axes (a, b, c) and the angles between them (α, β, γ). Each system has characteristic symmetry elements that determine possible crystal forms.
The Seven Systems¶
| System | Axes | Angles | Example Gems |
|---|---|---|---|
| Cubic | a = b = c | α = β = γ = 90° | Diamond, Spinel, Garnet |
| Hexagonal | a₁ = a₂ = a₃ ≠ c | α = β = 90°, γ = 120° | Beryl, Apatite |
| Trigonal | a₁ = a₂ = a₃ ≠ c | α = β = 90°, γ = 120° | Quartz, Ruby, Tourmaline |
| Tetragonal | a = b ≠ c | α = β = γ = 90° | Zircon, Rutile |
| Orthorhombic | a ≠ b ≠ c | α = β = γ = 90° | Topaz, Peridot |
| Monoclinic | a ≠ b ≠ c | α = γ = 90°, β ≠ 90° | Kunzite, Orthoclase |
| Triclinic | a ≠ b ≠ c | α ≠ β ≠ γ ≠ 90° | Turquoise, Labradorite |
Optic Character¶
| System | Optic Character | RI Values |
|---|---|---|
| Cubic | Isotropic | Single RI (n) |
| Hexagonal, Trigonal, Tetragonal | Uniaxial | Two values (ω, ε) |
| Orthorhombic, Monoclinic, Triclinic | Biaxial | Three values (α, β, γ) |
Data source: learn/crystal-systems.yaml