Rock Identifier
Banded agate (likely a small polished agate cabochon) (Microcrystalline quartz, chiefly SiO₂; banding is chalcedony with contrasting mineral inclusions or layers) — gemstone
gemstone

Banded agate (likely a small polished agate cabochon)

Microcrystalline quartz, chiefly SiO₂; banding is chalcedony with contrasting mineral inclusions or layers

AI-generated identification · may be incorrect

Polished, rounded stone with pale gray-white and dark gray/black bands. Quartz hardness 6.5–7 Mohs; vitreous to waxy luster, cryptocrystalline structure, no visible cleavage; specific gravity about 2.6.

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Physical properties

Polished, rounded stone with pale gray-white and dark gray/black bands. Quartz hardness 6.5–7 Mohs; vitreous to waxy luster, cryptocrystalline structure, no visible cleavage; specific gravity about 2.6.

Formation & geological history

Agate forms as silica-rich fluids deposit successive layers in cavities, commonly in volcanic rocks; the specimen’s geological age and exact source cannot be determined from the photo. The reported Tamil Nadu location is regionally plausible for quartz and agate-bearing material, though not enough to establish provenance.

Uses & applications

Used for jewelry, beads, cabochons, ornaments, and collecting; this small piece appears shaped and polished for jewelry or craft use.

Geological facts

Agate’s bands record changing silica deposition conditions; some bands become visible only after cutting and polishing.

Field identification & locations

Look for curved or parallel bands, a smooth polish, and hardness sufficient to scratch glass; visual identification alone cannot rule out dyed or imitation material. Similar agates occur worldwide, including India.