Rock Identifier
Dyed Agate (Microcrystalline Quartz (SiO2) with artificial pigment) — sedimentary
sedimentary

Dyed Agate

Microcrystalline Quartz (SiO2) with artificial pigment

Hardness: 6.5-7 (Mohs scale), Color: artificially bright magenta/pink, Lustre: Vitreous/Waxy, Structure: Cryptocrystalline, Fracture: Conchoidal

Hardness
6
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 (Mohs scale), Color: artificially bright magenta/pink, Lustre: Vitreous/Waxy, Structure: Cryptocrystalline, Fracture: Conchoidal

Formation & geological history

Formed as secondary deposits of silica in volcanic or metamorphic host rocks. These specific specimens have been tumbled and chemically dyed to achieve an unnaturally vibrant pink color.

Uses & applications

Decorative use, gemstone tumbling, jewelry (beads/cabochons), and metaphysical collections.

Geological facts

While agate is naturally occurring, the neon-pink color seen here does not exist in nature. Agate is porous, allowing it to soak up chemical dyes that settle in the crystal layers.

Field identification & locations

Identify by the extreme saturation of color which often concentrates in cracks or bands. Found globally in volcanic regions like Brazil and Uruguay.