Rock Identifier
Faceted color-change gemstone, likely synthetic alexandrite or glass imitation (Alexandrite: chrysoberyl, BeAl₂O₄; exact identification requires gemological testing) — gemstone
gemstone

Faceted color-change gemstone, likely synthetic alexandrite or glass imitation

Alexandrite: chrysoberyl, BeAl₂O₄; exact identification requires gemological testing

AI-generated identification · may be incorrect

Small oval cabochon/faceted stone with purple-blue and vivid green color zoning or color change, transparent to translucent, vitreous luster. Chrysoberyl hardness is 8.5 Mohs, orthorhombic, with poor cleavage; the photograph alone cannot establish hardness, density, or natural origin.

Identified More gemstone
Explore Faceted color-change gemstone, likely synthetic alexandrite or glass imitation in the encyclopedia →

Identify your own rocks.

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

Physical properties

Small oval cabochon/faceted stone with purple-blue and vivid green color zoning or color change, transparent to translucent, vitreous luster. Chrysoberyl hardness is 8.5 Mohs, orthorhombic, with poor cleavage; the photograph alone cannot establish hardness, density, or natural origin.

Formation & geological history

Natural alexandrite forms in rare chromium-bearing metamorphic or pegmatitic environments, mainly in Russia, Sri Lanka, Brazil, and East Africa. Synthetic alexandrite and inexpensive simulants are common; geological age is not determinable from the image.

Uses & applications

Used in jewelry and collections; fine natural alexandrite can be extremely valuable, while synthetic material is decorative and comparatively inexpensive.

Geological facts

Alexandrite is famous for green in daylight and red-purple under incandescent light; this specimen’s apparent green-purple contrast may instead reflect lighting, inclusions, or a coated/synthetic stone.

Field identification & locations

Confirm with daylight/incandescent color-change testing, refractive index, specific gravity, microscope examination, and spectroscopy; avoid scratch testing. Its polished oval shape suggests a jewelry stone rather than a raw mineral specimen.