A frieze group is a discrete subgroup of Euclidean isometries whose translation subgroup is generated by one nonzero vector and has finite index. A plane crystallographic group is a discrete subgroup of Euclidean isometries with a rank-two translation lattice of finite index; equivalently its action has a compact fundamental region.
Here are three frieze groups, with explicit generators. The translation alone gives . Adding the vertical reflection in mathematics gives , the infinite dihedral group, since . Instead adding the horizontal reflection in mathematics gives , since . Their translation parts are exactly and their point parts have respectively one, two and two elements.
For plane crystallographic groups, let and . These generate . Adding the half-turn gives , with inversion on both translation generators. Adding the quarter-turn gives , with and . These are the translation, half-turn and square-rotation wallpaper groups. Integer translation vectors and a finite point part make each group a discrete subgroup; the unit square meets every orbit, establishing a cocompact group action.
For the final claim, suppose a Euclidean isometry has order five. An orientation-reversing planar isometry has finite order only when it is a reflection in mathematics, so is a rotation through , , about some centre. Write for its linear rotation part. If is a nonzero translation, conjugation gives . Thus contains translations by and by , where .
For a primitive fifth root , dividing by gives . Hence is irrational. The pigeonhole principle, applied to fractional parts of in equal intervals, gives integers with . Consequently contains nonidentity translations by tending to the identity. This contradicts the discrete subgroup hypothesis. There is no element of order five. This argument needs only the given nonzero translation, not a rank-two lattice.
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