Rock Identifier
Polished banded agate (Agate, microcrystalline quartz (SiO₂; chiefly chalcedony)) — mineral
mineral

Polished banded agate

Agate, microcrystalline quartz (SiO₂; chiefly chalcedony)

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; glossy polish, translucent-to-opaque gray and cream bands, with a rounded natural-looking inclusion. Quartz has a trigonal crystal structure, though agate’s microscopic crystals are not individually visible; specific gravity about 2.6.

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Physical properties

Hardness 6.5–7 Mohs; glossy polish, translucent-to-opaque gray and cream bands, with a rounded natural-looking inclusion. Quartz has a trigonal crystal structure, though agate’s microscopic crystals are not individually visible; specific gravity about 2.6.

Formation & geological history

Silica-rich groundwater deposited successive chalcedony layers in a cavity, likely in volcanic rock. Agates form across many geological ages; the specimen has been cut and polished.

Uses & applications

Used for jewelry, ornaments, and collecting; agate is also used for small decorative and precision objects.

Geological facts

Agate banding records changing conditions as silica precipitated, and some bands can reveal concentric or fortification patterns.

Field identification & locations

Look for waxy luster, translucency at thin edges, and curved or parallel bands; common sources include Brazil, Uruguay, India, and the United States. The pictured polished piece is too small and lacks detail for a precise variety identification.