Most minerals are composed of two or more elements with their atoms arranged in a regular structure, called a crystal lattice or crystal structure. In chemistry, this is known as a compound. To visualize crystal structure, think of balls attached to other balls with sticks to make regular three-dimensional patterns. The balls represent atoms and the sticks represent the forces between the atoms. Electromagnetic forces between atoms hold some chemical compounds together. In other compounds, the atoms form covalent bonds, which means they share electrons. Scientists classify many minerals into groups based on the types of atoms found in the minerals. For example, oxides consist of metallic atoms bound to oxygen atoms, and sulfides are combinations of metal and sulfur atoms.

Pegmatites are extremely coarse-grained intrusive igneous rocks, containing crystals that are both large (at least 5 cm or 2 inches across) and packed closely together. Pegmatites crystallize during the final stages of granite formation. The same silicate minerals that form granite - quartz, feldspar, and mica - generally make up the bulk of pegmatites, too, but the individual minerals in pegmatites can be many centimeters or even several meters in diameter. Some pegmatites also contain less common minerals, such as garnet, albite, lepidolite, beryl, and fluorite. Geologists and miners sometimes find beautiful, gemstone-quality crystals of topaz, beryl (aquamarine), rose quartz, smoky quartz, and other minerals within pegmatites.