Rock Identifier
Brown agate or chalcedony cabochon pendant (Microcrystalline quartz (SiO₂), likely brown chalcedony/agate) — gemstone
gemstone

Brown agate or chalcedony cabochon pendant

Microcrystalline quartz (SiO₂), likely brown chalcedony/agate

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; opaque to slightly translucent brown, with a waxy-to-glassy luster and no visible cleavage. The smooth domed cabochon and metal setting obscure internal banding or crystal structure.

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Physical properties

Hardness 6.5–7 Mohs; opaque to slightly translucent brown, with a waxy-to-glassy luster and no visible cleavage. The smooth domed cabochon and metal setting obscure internal banding or crystal structure.

Formation & geological history

Chalcedony forms when silica-rich groundwater fills cavities and fractures, commonly in volcanic rocks; coloration may result from iron or other trace impurities. The specimen is polished and set in jewelry, so its precise geological age and locality cannot be determined visually.

Uses & applications

Used primarily in pendants, cabochons, carvings, and ornamental objects; durable enough for everyday jewelry. The surrounding setting appears to be silver-tone metal, possibly sterling silver, but requires testing.

Geological facts

Brown chalcedony is often marketed as smoky agate, brown agate, or chocolate chalcedony, though trade names are not always mineralogically precise. Lack of visible banding makes exact identification uncertain from the photograph alone.

Field identification & locations

Identify by its fine-grained waxy appearance, high hardness, and absence of cleavage; glass or plastic imitations may show bubbles, seams, or lower hardness. Common sources include Brazil, Uruguay, India, Mexico, Madagascar, and the United States.