Rock Identifier
Druzy chalcedony pendant, likely coated or dyed (Microcrystalline quartz (SiO₂), chalcedony with druzy quartz; surface may have titanium or metallic coating) — gemstone
gemstone

Druzy chalcedony pendant, likely coated or dyed

Microcrystalline quartz (SiO₂), chalcedony with druzy quartz; surface may have titanium or metallic coating

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; dark blue-purple iridescent color, vitreous-to-sparkling luster, granular quartz crystals, no obvious cleavage, and specific gravity about 2.6. The uniform rainbow sheen strongly suggests an artificial coating rather than natural color.

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Physical properties

Hardness about 6.5–7 Mohs; dark blue-purple iridescent color, vitreous-to-sparkling luster, granular quartz crystals, no obvious cleavage, and specific gravity about 2.6. The uniform rainbow sheen strongly suggests an artificial coating rather than natural color.

Formation & geological history

Chalcedony forms when silica-rich groundwater fills cavities and deposits microcrystalline quartz, commonly in volcanic rocks; associated host material may be Cenozoic to older. The pendant has been cut, polished, drilled, mounted, and likely coated or dyed.

Uses & applications

Used primarily in inexpensive jewelry and decorative cabochons; not generally used structurally or industrially in this form.

Geological facts

Druzy is a surface covered with tiny crystals, producing glitter under light. Titanium-coated quartz and coated druzy are often marketed under trade names such as “aura druzy.”

Field identification & locations

Identify by the sparkling crystalline surface, conchoidal-looking chalcedony base, and strong artificial iridescence; natural untreated druzy usually has more limited, uneven colors. Common sources include Brazil, Uruguay, Mexico, and Madagascar.