
mineral
Dzi Bead (Agate)
Chalcedony (cryptocrystalline variety of Quartz), SiO2
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Dark brown to black base with white etched patterns including circles (eyes) and geometric lines; Luster: Waxy to vitreous; Structure: Cryptocrystalline; Cleavage: None
- Hardness
- 6
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Dark brown to black base with white etched patterns including circles (eyes) and geometric lines; Luster: Waxy to vitreous; Structure: Cryptocrystalline; Cleavage: None
Formation & geological history
Formed as volcanic agate nodules through silica precipitation in rock cavities. These specific specimens are human-altered through ancient or modern chemical etching and baking processes to create permanent symbolic patterns.
Uses & applications
Used primarily in jewelry, as protective amulets, and as highly valued cultural artifacts in Himalayan regions; significant value in the antique and collectible market.
Geological facts
Dzi beads are considered sacred in Tibetan culture, often called 'Heaven's Pearls'. 'Eye' patterns are the most desirable, with certain counts (like 9-eyed beads) being incredibly auspicious and rare.
Field identification & locations
Look for 'weathering' marks (crescent-shaped indentations) and internal banding typical of agate. Modern replicas are common; authentic ancient beads have patterns that penetrate deep into the stone. Commonly found in Tibet, Bhutan, and the Himalayas.
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