crystal

Also known as crystalline solid

thumb|upright=1.25|Crystals of amethyst [[quartz]] thumb|upright=1.25|Microscopically, a single crystal has atoms in a near-perfect periodic arrangement; a polycrystal is composed of many microscopic crystals (called "[[crystallites" or "grains"); and an amorphous solid (such as glass) has no periodic arrangement even microscopically.]]

AI overview

A crystal is a solid material in which atoms are arranged in a highly ordered, repeating pattern throughout the structure. Crystals matter because their atomic organization gives them distinctive properties—such as specific shapes, hardness, and optical qualities—that make them useful in everything from jewelry to electronics and scientific research.

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Wikidata facts

Image: Quartz oisan.jpg

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Commons gallery: Crystal
Commons category: Crystals
P8168: Q254906
exact match: purl.obolibrary.org/obo/ENVO_01000845

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~22 min read

Article

17 sections

Contents

Crystal structure (microscopic)
Crystal faces, shapes and crystallographic forms
Occurrence in nature
Rocks
Ice
Organigenic crystals
Polymorphism and allotropy
Crystallization
Defects, impurities, and twinning
Chemical bonds
Quasicrystals
Special properties from anisotropy
Crystallography
Image gallery
See also
References
Further reading

A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions. In addition, macroscopic single crystals are usually identifiable by their geometrical shape, consisting of flat faces with specific, characteristic orientations. The scientific study of crystals and crystal formation is known as crystallography. The process of crystal formation via mechanisms of crystal growth is called crystallization or solidification.