Rock Identifier
Lapis Lazuli (Lapis Lazuli (Rock containing Lazurite, Na8[AlSi O4]6[S,Cl,SO4,OH]2)) — metamorphic
metamorphic

Lapis Lazuli

Lapis Lazuli (Rock containing Lazurite, Na8[AlSi O4]6[S,Cl,SO4,OH]2)

Hardness: 5 to 5.5 (Mohs scale), Color: Deep blue to violet-blue, Luster: Vitreous to greasy, Crystal structure: Isometric (Lazurite component), Cleavage: Indistinct, Specific Gravity: 2.7 to 2.9

Hardness
5 to 5
Identified More metamorphic

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Physical properties

Hardness: 5 to 5.5 (Mohs scale), Color: Deep blue to violet-blue, Luster: Vitreous to greasy, Crystal structure: Isometric (Lazurite component), Cleavage: Indistinct, Specific Gravity: 2.7 to 2.9

Formation & geological history

Formed through contact metamorphism, primarily in crystalline limestones. The blue color comes from the mineral lazurite. It has been mined for over 6,000 years, notably in the Sar-e-Sang mines in Afghanistan.

Uses & applications

Used in gemstone jewelry (cabochons and beads), decorative carvings, high-end tiling, and historically as a pigment (Ultramarine blue) for fine arts painting.

Geological facts

In ancient Egypt, it was a favorite stone for amulets and ornaments, including the burial mask of Tutankhamun. Michelangelo used pulverized lapis to paint the ceiling of the Sistine Chapel.

Field identification & locations

Identify by its 'royal blue' color often accompanied by gold-colored pyrite specks (flecks) and white calcite veins. Commonly found in Afghanistan, Chile, Russia, and Myanmar.