Rock Identifier
Lapis Lazuli (Low-grade/Calcite-heavy) (Na8[Al6Si6O24]n(S,Cl,SO4,OH)2 (Lazurite component)) — metamorphic
metamorphic

Lapis Lazuli (Low-grade/Calcite-heavy)

Na8[Al6Si6O24]n(S,Cl,SO4,OH)2 (Lazurite component)

Hardness: 5-5.5 (Mohs scale); Color: Azure blue mottled with white and grey; Luster: Vitreous to greasy; Crystal Structure: Isometric; Specific Gravity: 2.7-2.9

Hardness
5-5
Color
Azure blue mottled with white and grey
Luster
Vitreous to greasy
Identified More metamorphic

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Physical properties

Hardness: 5-5.5 (Mohs scale); Color: Azure blue mottled with white and grey; Luster: Vitreous to greasy; Crystal Structure: Isometric; Specific Gravity: 2.7-2.9

Formation & geological history

Formed via contact metamorphism, typically when limestone or marble is altered by heat and pressure from magmatic intrusions. Often found in deposits billions of years old.

Uses & applications

Primarily used in jewelry for beads and cabochons, decorative carvings, and historically as a pigment for ultramarine paint.

Geological facts

The blue color comes from the sulfur in the lazurite mineral; the white inclusions in these beads are calcite, and the grey/metallic bits are likely pyrite.

Field identification & locations

Identified by its distinctive deep blue color paired with white calcite mottling. Major sources include the Sar-e-Sang mines in Afghanistan, as well as Russia and Chile.