Rock Identifier
Polished red chalcedony (likely dyed agate) (Chalcedony, microcrystalline quartz (SiO₂), possibly colored by iron oxides or dye) — gemstone
gemstone

Polished red chalcedony (likely dyed agate)

Chalcedony, microcrystalline quartz (SiO₂), possibly colored by iron oxides or dye

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; translucent to opaque red with a waxy-to-glassy luster, cryptocrystalline structure, and no visible cleavage. The smooth, polished surface and possible banding are typical of agate/chalcedony.

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Physical properties

Hardness 6.5–7 Mohs; translucent to opaque red with a waxy-to-glassy luster, cryptocrystalline structure, and no visible cleavage. The smooth, polished surface and possible banding are typical of agate/chalcedony.

Formation & geological history

Forms when silica-rich groundwater fills cavities in volcanic rocks, depositing successive layers of microcrystalline quartz over millions of years, commonly during the Cenozoic or older volcanic episodes. Strong uniform red color may indicate human dyeing or enhancement.

Uses & applications

Used for cabochons, carvings, ornamental slabs, jewelry, and decorative objects; common polished pieces have modest collector value.

Geological facts

Chalcedony is quartz whose crystals are too small to see unaided; agate is a banded variety. Dye concentrations in cracks, pores, or along edges can distinguish treated material from naturally colored stone.

Field identification & locations

Common sources include Brazil, Uruguay, India, Madagascar, Mexico, and the United States. Test with a loupe for curved or parallel banding, inspect color concentration at fractures, and avoid acid or scratch testing on the polished face.