Rock Identifier
Blue stone cabochon, likely lapis lazuli or dyed stone (Lapis lazuli: lazurite-rich rock, chiefly (Na,Ca)₈(AlSiO₄)₆(S,SO)₂; exact identification is uncertain from the image) — gemstone
gemstone

Blue stone cabochon, likely lapis lazuli or dyed stone

Lapis lazuli: lazurite-rich rock, chiefly (Na,Ca)₈(AlSiO₄)₆(S,SO)₂; exact identification is uncertain from the image

AI-generated identification · may be incorrect

Small polished, faceted blue piece with medium luster and apparently opaque texture. Lapis lazuli typically has Mohs hardness 5–5.5, deep ultramarine color, and may contain white calcite and metallic pyrite specks.

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Physical properties

Small polished, faceted blue piece with medium luster and apparently opaque texture. Lapis lazuli typically has Mohs hardness 5–5.5, deep ultramarine color, and may contain white calcite and metallic pyrite specks.

Formation & geological history

Natural lapis lazuli forms by contact metamorphism of limestone, commonly in Precambrian deposits; notable material comes from Afghanistan, Chile, and Siberia. The specimen appears cut or polished rather than naturally crystallized.

Uses & applications

Used for cabochons, beads, carvings, ornaments, and historically as the ultramarine pigment source. Lower-grade blue stones may be dyed jasper, sodalite, or glass substitutes.

Geological facts

True lapis commonly shows uneven blue color with calcite veining or pyrite flecks; uniformly vivid blue material can be treated or synthetic. It is a rock rather than a single mineral.

Field identification & locations

Check for natural variation, white calcite, and brassy pyrite; a glassy appearance, bubbles, or perfectly uniform color suggests imitation. A scratch test and magnification help, but laboratory testing is preferable.