Rock Identifier
Polished banded agate (probable) (Microcrystalline quartz, SiO₂ (chalcedony/agate)) — mineral
mineral

Polished banded agate (probable)

Microcrystalline quartz, SiO₂ (chalcedony/agate)

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; translucent gray, cream, brown, and black curved banding with a vitreous to waxy luster. Agate is cryptocrystalline quartz and commonly has no visible cleavage; specific gravity is about 2.6.

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Physical properties

Hardness 6.5–7 Mohs; translucent gray, cream, brown, and black curved banding with a vitreous to waxy luster. Agate is cryptocrystalline quartz and commonly has no visible cleavage; specific gravity is about 2.6.

Formation & geological history

Forms when silica-rich groundwater fills cavities in volcanic rock, depositing successive chalcedony and quartz bands. Individual bands may range from Paleozoic to recent in age, depending on the host rock and locality.

Uses & applications

Cut and polished for cabochons, beads, ornaments, bookends, and lapidary specimens; its durability makes it suitable for jewelry and decorative objects.

Geological facts

The dark areas may be iron- or manganese-rich inclusions, or natural dendritic patterns; dyeing is also common in commercial agate, though this piece’s colors appear plausibly natural.

Field identification & locations

Identify by curved or concentric banding, translucency, waxy polish, and resistance to scratching with steel. Common sources include Brazil, Uruguay, Mexico, India, Madagascar, and the United States.