Rock Identifier
Polished black-and-white banded agate (likely dyed or painted) (Chalcedony (microcrystalline quartz), SiO₂; exact banding variety uncertain) — gemstone
gemstone

Polished black-and-white banded agate (likely dyed or painted)

Chalcedony (microcrystalline quartz), SiO₂; exact banding variety uncertain

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; vitreous to waxy luster, opaque black and white bands, cryptocrystalline quartz, no visible cleavage, specific gravity about 2.60–2.65. The regular high-contrast pattern and polish suggest human processing; it may be a carved bead or pendant component.

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Physical properties

Hardness about 6.5–7 Mohs; vitreous to waxy luster, opaque black and white bands, cryptocrystalline quartz, no visible cleavage, specific gravity about 2.60–2.65. The regular high-contrast pattern and polish suggest human processing; it may be a carved bead or pendant component.

Formation & geological history

Agate forms when silica-rich groundwater fills cavities in volcanic rocks, commonly during the Paleozoic–Cenozoic; individual specimen age and locality cannot be determined from the image.

Uses & applications

Used for beads, ornaments, cabochons, and carvings; generally decorative rather than high-value jewelry material.

Geological facts

Black coloration may result from natural manganese/iron compounds, dye, or surface paint. The adjacent brown object appears separate and is not identified here.

Field identification & locations

Look for curved/concentric banding, waxy luster, quartz-like hardness, and inability to scratch it with a steel knife; glass or paint may scratch or chip. Common sources include Brazil, Uruguay, India, Madagascar, and Mexico.