Minerals can be identified by the shape of their crystals or crystallography. The shapes of crystals are determined by a number of factors such as the size and length of their surfaces (known as 'faces') and edges, as well as the angles between these. These shapes are named after their geometry - for example, crystals based on cubes belong to the 'cubic or isometric' crystal group. There are seven main crystal groups or systems, as shown here. These are ordered from most symmetrical to least symmetrical.


Main crystal groups or systems - most to least symmetrical

Crystal group 1: Cubic (Isometric)


Crystal group 2: Tetragonal


Crystal group 3: Hexagonal


Crystal group 4: Trigonal


Crystal group 5: Orthorhombic


Crystal group 6: Monoclinic


Crystal group 7: Triclinic