
mineral
Polished agate (likely carnelian/mossy chalcedony)
Chalcedony, microcrystalline quartz (SiO₂), with iron-oxide banding and possible inclusions
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; dark gray-green to brown with a reddish-brown band, waxy to vitreous luster, cryptocrystalline structure, and no visible cleavage. The rounded shape indicates tumbling or natural water wear.
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Physical properties
Hardness 6.5–7 Mohs; dark gray-green to brown with a reddish-brown band, waxy to vitreous luster, cryptocrystalline structure, and no visible cleavage. The rounded shape indicates tumbling or natural water wear.
Formation & geological history
Forms when silica-rich groundwater fills cavities in volcanic rock, depositing chalcedony in successive bands; iron produces red-brown coloration. Individual bands may form over long intervals, commonly in Cenozoic volcanic terrains.
Uses & applications
Used for cabochons, beads, carvings, ornaments, and lapidary specimens; durable enough for some decorative and functional objects.
Geological facts
Agate is a variety of chalcedony defined by banding or patterned coloration. This specimen may also be sold as “black agate,” though its exact variety cannot be confirmed from the photograph alone.
Field identification & locations
Identify by its hardness, waxy luster, translucency at thin edges, and curved internal banding; it should resist scratching by a steel blade. Common sources include Brazil, Uruguay, India, Madagascar, Mexico, and the western United States.
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