Rock Identifier
Tumbled ruby-bearing corundum (likely dyed or fracture-filled) (Corundum, aluminum oxide (Al₂O₃), with chromium producing ruby-red color) — gemstone
gemstone

Tumbled ruby-bearing corundum (likely dyed or fracture-filled)

Corundum, aluminum oxide (Al₂O₃), with chromium producing ruby-red color

AI-generated identification · may be incorrect

Mohs hardness 9; vivid pink-purple to magenta color, vitreous luster, translucent body with fractures and cloudy inclusions. Corundum has a trigonal crystal structure and no true cleavage, though it commonly fractures conchoidally or unevenly.

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Physical properties

Mohs hardness 9; vivid pink-purple to magenta color, vitreous luster, translucent body with fractures and cloudy inclusions. Corundum has a trigonal crystal structure and no true cleavage, though it commonly fractures conchoidally or unevenly.

Formation & geological history

Natural ruby forms when aluminum-rich rocks undergo metamorphism or crystallize in igneous/metasomatic environments; ruby-bearing deposits range from Precambrian to younger ages. The intense purple color and uniform appearance may indicate dyeing or treatment, common in commercial tumbled stones.

Uses & applications

Used as an abrasive and, when transparent and intensely red, as a gemstone; opaque tumbled material is mainly decorative and collectible.

Geological facts

Ruby and sapphire are color varieties of the same mineral, corundum; chromium causes red coloration, while purple tones can involve chromium, vanadium, or treatment.

Field identification & locations

Test cautiously: corundum resists scratching by steel and quartz, but a scratch test can damage polished material. Common sources include Myanmar, Mozambique, Sri Lanka, India, Tanzania, and Madagascar; the specimen’s appearance is not sufficient to confirm natural ruby.