Rock Identifier
Red corundum (ruby) crystal fragment (Corundum, Al₂O₃; ruby is red corundum colored mainly by chromium) — gemstone
gemstone

Red corundum (ruby) crystal fragment

Corundum, Al₂O₃; ruby is red corundum colored mainly by chromium

AI-generated identification · may be incorrect

The small vivid-red fragment appears translucent with a vitreous luster, but the photo is insufficient to confirm its identity. Corundum has Mohs hardness 9, a trigonal crystal structure, no true cleavage, and specific gravity around 4.0.

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Physical properties

The small vivid-red fragment appears translucent with a vitreous luster, but the photo is insufficient to confirm its identity. Corundum has Mohs hardness 9, a trigonal crystal structure, no true cleavage, and specific gravity around 4.0.

Formation & geological history

Natural ruby forms in aluminum-rich, silica-poor metamorphic rocks or in some igneous settings; gem deposits range from ancient to geologically recent. A red fragment may also be synthetic or treated.

Uses & applications

Rubies are cut for jewelry and collected; corundum is also used as an abrasive and in hard-wearing components.

Geological facts

Ruby and sapphire are varieties of the same mineral, corundum; trace elements determine color.

Field identification & locations

Check for hardness, crystal form, and diagnostic inclusions, but these require testing; red glass or synthetic corundum can look similar. Natural rubies occur in Myanmar, Mozambique, Sri Lanka, Thailand, and elsewhere.