
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 incorrectGlossy, 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.
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