Rock Identifier
Red corundum (ruby-colored polished crystal) (Corundum, aluminum oxide (Al₂O₃); red color is typically caused by chromium) — gemstone
gemstone

Red corundum (ruby-colored polished crystal)

Corundum, aluminum oxide (Al₂O₃); red color is typically caused by chromium

AI-generated identification · may be incorrect

Mohs hardness 9, vitreous luster, deep red color, trigonal crystal structure, and no true cleavage. The pointed, polished form and uniform translucency suggest a cut or synthetic specimen; visual identification cannot confirm natural origin.

Identified More gemstone
Explore Red corundum (ruby-colored polished crystal) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Mohs hardness 9, vitreous luster, deep red color, trigonal crystal structure, and no true cleavage. The pointed, polished form and uniform translucency suggest a cut or synthetic specimen; visual identification cannot confirm natural origin.

Formation & geological history

Corundum forms in aluminum-rich metamorphic rocks and some igneous deposits; ruby-bearing rocks commonly formed during Precambrian to younger metamorphic events. Synthetic ruby is produced industrially by flame-fusion or hydrothermal methods.

Uses & applications

Used as an abrasive and in scratch-resistant components; gem-quality natural ruby is used in jewelry, while synthetic ruby is common for ornaments, lasers, and watch bearings.

Geological facts

Ruby is the red variety of corundum; other colors are called sapphire. The specimen’s intense uniform color and unusually smooth elongated shape may indicate synthetic ruby or dyed glass rather than natural ruby.

Field identification & locations

Test hardness, refractive index, inclusions, and chemistry; a gem laboratory is needed to distinguish natural ruby from synthetic material or glass. Natural ruby occurs notably in Myanmar, Mozambique, Sri Lanka, and Tanzania.