
metamorphic
Lapis lazuli
Lazurite-rich lapis lazuli; chiefly lazurite (Na₃CaAl₃Si₃O₁₂S), with calcite and commonly pyrite
AI-generated identification · may be incorrectThe upper specimen appears to be rough, gray-blue lapis; the lower piece is polished deep-blue lapis. Lazurite has Mohs hardness 5–5.5 and a glassy-to-dull luster; lapis is an aggregate with variable hardness and no consistent cleavage.
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Physical properties
The upper specimen appears to be rough, gray-blue lapis; the lower piece is polished deep-blue lapis. Lazurite has Mohs hardness 5–5.5 and a glassy-to-dull luster; lapis is an aggregate with variable hardness and no consistent cleavage.
Formation & geological history
Lapis forms through contact metamorphism of limestone, often in Precambrian rocks. The label indicates Afghanistan, whose deposits formed in the Sar-e-Sang region of Badakhshan.
Uses & applications
Used for beads, cabochons, carvings, decorative objects, and historically as the ultramarine pigment. Polished material is valued in jewelry and ornament.
Geological facts
The vivid blue color comes mainly from sulfur-bearing lazurite; gold-colored flecks, when present, are usually pyrite, not gold.
Field identification & locations
Identify by its intense blue color, opaque appearance, and possible white calcite or brassy pyrite flecks; Afghan lapis is especially renowned. The image supports a likely identification, though color alone cannot confirm composition.
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