Rock Identifier
Dyed agate slice (Microcrystalline quartz (SiO₂), typically banded chalcedony) — mineral
mineral

Dyed agate slice

Microcrystalline quartz (SiO₂), typically banded chalcedony

AI-generated identification · may be incorrect

Blue-green, translucent to opaque center with a darker rough rim; quartz has Mohs hardness 6.5–7, vitreous to waxy luster, and no cleavage. The visible coloration may be artificial; the image does not show clear natural banding.

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Physical properties

Blue-green, translucent to opaque center with a darker rough rim; quartz has Mohs hardness 6.5–7, vitreous to waxy luster, and no cleavage. The visible coloration may be artificial; the image does not show clear natural banding.

Formation & geological history

Agate forms as silica-rich fluids deposit chalcedony in cavities, commonly in volcanic rocks, over geological time. This appears cut and likely dyed or otherwise treated; its exact source and age cannot be determined from the image.

Uses & applications

Decorative slice, jewelry component, or collectible; agate is also used for ornaments and small craft objects.

Geological facts

Agate is a variety of chalcedony, composed of extremely fine quartz crystals; porous agate is often dyed to produce vivid colors.

Field identification & locations

Look for concentric bands, translucent chalcedony, and a contrasting outer rind; treatment can make color unreliable for identification. Agate occurs worldwide, including Brazil, Uruguay, India, and the United States.