
metamorphic
Polished ruby-in-zoisite (anyolite), probable
Ruby-bearing zoisite; zoisite Ca₂Al₃(SiO₄)₃(OH), with corundum Al₂O₃
AI-generated identification · may be incorrectSmall polished cabochon with dark green, opaque-to-translucent zoisite and vivid pink-red ruby inclusions. Zoisite has Mohs hardness 6–7 and vitreous luster; ruby is hardness 9, with no cleavage and trigonal crystal structure. Exact identification is visual and would benefit from testing.
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Physical properties
Small polished cabochon with dark green, opaque-to-translucent zoisite and vivid pink-red ruby inclusions. Zoisite has Mohs hardness 6–7 and vitreous luster; ruby is hardness 9, with no cleavage and trigonal crystal structure. Exact identification is visual and would benefit from testing.
Formation & geological history
Formed by regional metamorphism of aluminum-rich rocks, commonly in East African metamorphic terrains; notable material comes from Tanzania and Kenya. The geological age varies by deposit, commonly Precambrian.
Uses & applications
Used for cabochons, carvings, beads, and mineral specimens; attractive pieces have modest jewelry value. Green zoisite is also used decoratively, while ruby inclusions provide color contrast.
Geological facts
The trade name “anyolite” generally refers to ruby-bearing green zoisite, especially Tanzanian material. Ruby may appear as pink, red, or purplish patches rather than transparent gem crystals.
Field identification & locations
Identify by the green matrix, contrasting pink-red ruby, opaque appearance, and relatively soft polish compared with ruby. Common sources include Tanzania, Kenya, and occasionally Norway; hardness, streak, and magnification can help distinguish it from dyed jade or glass.
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