gemstone

Likely raw emerald or green beryl

Beryl, Be₃Al₂Si₆O₁₈; green color typically from chromium or vanadium

AI-generated identification · may be incorrect

Small opaque-to-translucent, granular green crystal with vitreous-to-dull luster; beryl has Mohs hardness 7.5–8, hexagonal crystal structure, no prominent cleavage, and specific gravity about 2.63–2.92.

Identified August 30, 2026More gemstone →

Explore Likely raw emerald or green beryl in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Formation & geological history

Forms mainly in hydrothermal pegmatites and metamorphic zones when beryllium-rich fluids interact with chromium- or vanadium-bearing rocks. Most gem emerald is Paleozoic to younger, though age varies by deposit.

Uses & applications

Gem-quality material is cut for jewelry; lower-grade specimens are collected or used decoratively. This piece appears small and heavily included, limiting commercial gem use.

Geological facts

The photograph alone cannot distinguish emerald from other green minerals such as nephrite, serpentine, aventurine, or green tourmaline. Emerald is defined by beryl composition, not simply by green color.

Field identification & locations

Common sources include Colombia, Zambia, Brazil, Ethiopia, Pakistan, and Afghanistan. Confirm with hardness, refractive index, specific gravity, and ideally Raman or chemical testing; avoid scratching the specimen unnecessarily.