
mineral
Rough ruby-bearing corundum (identification uncertain)
Corundum (Al₂O₃), possibly ruby; the image alone cannot confirm ruby or distinguish it from other red-purple minerals.
AI-generated identification · may be incorrectAppears opaque and rough, with red-purple areas and gray/yellow matrix. Corundum has Mohs hardness 9, a trigonal crystal structure, and no true cleavage; luster is vitreous to dull when unpolished.
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Physical properties
Appears opaque and rough, with red-purple areas and gray/yellow matrix. Corundum has Mohs hardness 9, a trigonal crystal structure, and no true cleavage; luster is vitreous to dull when unpolished.
Formation & geological history
Corundum forms in aluminum-rich, silica-poor metamorphic rocks and some igneous settings; age depends on the deposit. The specimen may be corundum-bearing host rock, but its origin is not determinable from the photo.
Uses & applications
Gem-quality ruby is used in jewelry; industrial corundum is an abrasive and refractory material. This rough piece has no obvious gem value from the image.
Geological facts
Ruby is the red variety of corundum, with color chiefly caused by chromium. Color alone is not sufficient to identify it.
Field identification & locations
Check hardness, crystal habit, and mineral composition; reliable identification usually requires testing or laboratory analysis. Rubies occur notably in Myanmar, Mozambique, Madagascar, and Sri Lanka.
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