In crystallography, the orthorhombic crystal system is one of the 7 lattice point groups. Orthorhombic lattices result from stretching a cubic lattice along two of its lattice vectors by two different factors, resulting in a rectangular prism with a rectangular base (a by b, which is different from a) and height (c, which is different from a and b). All three bases intersect at 90° angles. The three lattice vectors remain mutually orthogonal.
There are four orthorhombic Bravais lattices: simple orthorhombic, base-centered orthorhombic, body-centered orthorhombic, and face-centered orthorhombic.
| simple orthorhombic | base-centered orthorhombic | body-centered orthorhombic | face-centered orthorhombic |
The point groups (or crystal classes) that fall under this crystal system are listed below, followed by their representations in international notation and Schoenflies notation, and mineral examples.
| name | international | Schoenflies | example |
| orthorhombic bipyramidal | D2h | sulfur | |
| orthorhombic pyramidal | C2v | ||
| orthorhombic sphenoidal | D2 |
Orthorhombisches Kristallsystem | Rombiline süngoonia | 사방정계 | Ortorrômbico | Ромбическая сингония | 斜方晶系
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"Orthorhombic crystal system".
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