Mineral crystals form through the process of atoms bonding together in an orderly structure. There are three main ways minerals form: (1) from precipitation in hot water as the solution cools and atoms bond, (2) from magma as it cools below the solidification point of different minerals and they crystallize out, and (3) through evaporation of water leaving behind mineral deposits. The rate of crystal growth depends on temperature, pressure, and the atoms available in the surrounding environment.