Rock Identifier
Polished agate (likely carnelian/mossy chalcedony) (Chalcedony, microcrystalline quartz (SiO₂), with iron-oxide banding and possible inclusions) — mineral
mineral

Polished agate (likely carnelian/mossy chalcedony)

Chalcedony, microcrystalline quartz (SiO₂), with iron-oxide banding and possible inclusions

AI-generated identification · may be incorrect

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.

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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.