
metamorphic
Polished multicolored mineral pebble, possibly ruby-in-zoisite
Ruby-bearing zoisite (zoisite: Ca₂Al₃(SiO₄)₃(OH); ruby: corundum, Al₂O₃)
AI-generated identification · may be incorrectSmall rounded specimen with a green-gray matrix and a pink-red inclusion, consistent with ruby-in-zoisite; zoisite has Mohs hardness 6–7, while ruby is 9. Typically vitreous to waxy luster, granular texture, and no obvious cleavage.
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Physical properties
Small rounded specimen with a green-gray matrix and a pink-red inclusion, consistent with ruby-in-zoisite; zoisite has Mohs hardness 6–7, while ruby is 9. Typically vitreous to waxy luster, granular texture, and no obvious cleavage.
Formation & geological history
Forms by metamorphism of aluminum- and calcium-rich rocks, commonly in East African deposits; geological ages vary by locality, often Precambrian. The rounded shape indicates tumbling or polishing rather than natural crystal faces.
Uses & applications
Used as a lapidary material for cabochons, beads, carvings, and decorative specimens; rarely used for high-value jewelry because the matrix is opaque and variable.
Geological facts
The red areas are ruby, the green matrix is zoisite, and black flecks may be hornblende or other accessory minerals. Strong color contrast is its defining visual feature.
Field identification & locations
Commonly identified by opaque green/gray zoisite containing contrasting pink-red ruby patches; a scratch test should not be used on a valuable specimen. Common sources include Tanzania and Kenya.
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