
mineral
Polished banded agate (likely carnelian and black agate)
Chalcedony, microcrystalline quartz (SiO₂), with iron-oxide coloration
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; waxy to vitreous luster; translucent reddish-brown and opaque dark-gray bands; cryptocrystalline, with no visible cleavage and conchoidal fracture. The smooth surface indicates a polished or tumbled specimen.
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Physical properties
Hardness 6.5–7 Mohs; waxy to vitreous luster; translucent reddish-brown and opaque dark-gray bands; cryptocrystalline, with no visible cleavage and conchoidal fracture. The smooth surface indicates a polished or tumbled specimen.
Formation & geological history
Forms when silica-rich groundwater fills cavities in volcanic rock, depositing successive layers of chalcedony; iron oxides create red-brown tones. Individual agates commonly formed during volcanic activity from the Paleozoic to Cenozoic eras.
Uses & applications
Used for cabochons, beads, carvings, paperweights, and decorative objects; durable and inexpensive compared with many gemstones.
Geological facts
Agate is a variety of chalcedony distinguished by banding or other patterned color zones. Red-orange areas are commonly called carnelian, while dark areas may be black chalcedony or iron/manganese-rich bands.
Field identification & locations
Identify it by its glassy-waxy polish, exceptional smoothness, fine banding, and hardness; it should resist scratching by steel but be scratched by quartz. Common sources include Brazil, Uruguay, India, Madagascar, Mexico, and the United States.
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