Rock Identifier
Tumbled black stone, likely black agate or onyx (Microcrystalline quartz (SiO₂), probably chalcedony/black agate; exact identification requires testing) — mineral
mineral

Tumbled black stone, likely black agate or onyx

Microcrystalline quartz (SiO₂), probably chalcedony/black agate; exact identification requires testing

AI-generated identification · may be incorrect

Glossy, smoothly tumbled, opaque black with a thin pale gray-white curved band. Quartz hardness is about 6.5–7 Mohs, vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, and specific gravity near 2.6.

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Physical properties

Glossy, smoothly tumbled, opaque black with a thin pale gray-white curved band. Quartz hardness is about 6.5–7 Mohs, vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, and specific gravity near 2.6.

Formation & geological history

Agate forms when silica-rich groundwater fills cavities in volcanic rock and deposits layered chalcedony; black coloration may result from iron, manganese, organic matter, or dyeing. Deposits range from Paleozoic to Cenozoic in age.

Uses & applications

Used for cabochons, beads, carvings, worry stones, and decorative objects; larger agate slabs are used ornamentally. Common tumbled pieces have modest value.

Geological facts

The pale line resembles agate banding, but black onyx, dyed chalcedony, or slag-like material can look similar. A glassy luster, cool feel, and lack of bubbles support quartz rather than glass.

Field identification & locations

Commonly found in Brazil, Uruguay, India, Madagascar, Mexico, and the United States. Check for banding under magnification, test hardness against glass, and inspect for dye concentration in cracks or pores.