Rock Identifier
Lapis lazuli (Lazurite-rich lapis lazuli; chiefly lazurite (Na₃CaAl₃Si₃O₁₂S), with calcite and commonly pyrite) — metamorphic
metamorphic

Lapis lazuli

Lazurite-rich lapis lazuli; chiefly lazurite (Na₃CaAl₃Si₃O₁₂S), with calcite and commonly pyrite

AI-generated identification · may be incorrect

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.

Identified More metamorphic
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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.