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Lazurite
Chemical Formula	(Na,Ca)8[(S,Cl,SO4,OH)2|(Al6Si6O24)]
Species	Silicates
Crystal System	Isometric
Mohs Scale	5
Specific Gravity	2.38-2.45
Color	Deep blue, azure, Purple-blue, greenish blue
Streak	Bright blue
Luster	Vitreous
Refractive Index	n = 1.502 - 1.522
Diaphaneity	Transparent, Opaque
Cleavage	Imperfect/FairImperfect on
Fracture	Irregular/Uneven
Crystal Habit：Crystals occur as dodecahedra, or rarely cubes; granular, disseminated, or massive
Geological Setting：Contact metamorphic mineral in limestones.

Lazurite is a tectosilicate mineral with sulfate, sulfur and chloride with formula: (Na,Ca)₈[(S,Cl,SO₄,OH)₂|(Al₆Si₆O₂₄)]. It is a feldspathoid and a member of the sodalite group. Lazurite crystallizes in the isometric system although well formed crystals are rare. It is usually massive and forms the bulk of the gemstone lapis lazuli.

Lazurite is a deep blue to greenish blue. The colour is due to the presence of S₃^- anions. It has a Mohs hardness of 5 to 5.5 and a specific gravity of 2.4. It is translucent with a refractive index of 1.50. It is fusible at 3.5 and soluble in HCl. It commonly contains or is associated with grains of pyrite.

Lazurite is a product of contact metamorphism of limestone and typically is associated with calcite, pyrite, diopside, humite, forsterite, hauyne and muscovite.

Other blue minerals such as the carbonate azurite and the phosphate lazulite may be confused with lazurite, but are easily distinguished with careful examination. Lazurite at one time was used as a synonym for azurite.

Lazurite was first described in 1890 for an occurrence in the Sar-e-Sang District, Koksha Valley, Badakhshan Province, Afghanistan. It has been mined for over 6,000 years in the lapis lazuli district of Badakhshan, Afghanistan. It has been used as a pigment in painting and cloth dyeing since at least the sixth or seventh century AD. It is also mined at Lake Baikal in Siberia; Mount Vesuvius; Burma; Canada; and the United States. The name is from the Persian lazward for blue.