Rock Identifier
Lapis Lazuli (Lazurite-rich metamorphic rock (approx. (Na,Ca)8(AlSiO4)6(S,Cl,SO4,OH)2)) — metamorphic
metamorphic

Lapis Lazuli

Lazurite-rich metamorphic rock (approx. (Na,Ca)8(AlSiO4)6(S,Cl,SO4,OH)2)

Hardness: 5-5.5 (Mohs scale), Color: Intense deep blue (often with gold pyrite or white calcite flecks), Luster: Vitreous to greasy, Crystal structure: Isometric (dodecahedral habits), Specific Gravity: 2.7-2.9

Hardness
5-5
Identified More metamorphic

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Physical properties

Hardness: 5-5.5 (Mohs scale), Color: Intense deep blue (often with gold pyrite or white calcite flecks), Luster: Vitreous to greasy, Crystal structure: Isometric (dodecahedral habits), Specific Gravity: 2.7-2.9

Formation & geological history

Formed via contact metamorphism of limestone or marble. The primary blue color comes from lazurite, formed in high-temperature environments. Most famous deposits are found in the Sar-e-Sang mines in Afghanistan which have been worked for over 6,000 years.

Uses & applications

Used primarily in jewelry, cabochons, and ornamental carvings. Historically crushed into powder for the pigment 'ultramarine' used in Renaissance paintings. Collectible for its deep pigment and pyrite inclusions.

Geological facts

Lapis lazuli was highly prized by the ancient Egyptians and was used in the funeral mask of Tutankhamun. It is technically a rock, not a mineral, because it is composed of several different minerals (lazurite, pyrite, and calcite).

Field identification & locations

Look for the signature 'royal blue' color with characteristic 'fools gold' (pyrite) inclusions. It will not scratch glass easily due to its moderate hardness. Commonly found in Afghanistan, Chile, Russia, and Canada.