
mineral
Polished agate (likely moss or plume agate)
Microcrystalline quartz, mainly chalcedony (SiO₂), with possible calcite or quartz vein inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; translucent gray-brown body with cream-white banding or vein-like inclusions, waxy to glassy luster, cryptocrystalline structure, and no obvious cleavage. The wet surface enhances translucency and gloss.
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Physical properties
Hardness about 6.5–7 Mohs; translucent gray-brown body with cream-white banding or vein-like inclusions, waxy to glassy luster, cryptocrystalline structure, and no obvious cleavage. The wet surface enhances translucency and gloss.
Formation & geological history
Forms when silica-rich groundwater fills cavities in volcanic rocks, depositing layers of chalcedony and quartz over time; individual bands may form over millions of years, commonly in Cenozoic to older volcanic terrains.
Uses & applications
Used for cabochons, beads, carvings, lapidary pieces, and inexpensive collectibles; durable polished agate is also used for decorative objects and occasional industrial bearings.
Geological facts
Agate’s patterns result from repeated changes in silica chemistry, impurities, and fluid flow. The specimen appears tumbled or naturally water-smoothed rather than freshly fractured.
Field identification & locations
Identify by its waxy translucency, curved or irregular banding, high hardness, and resistance to scratching by steel; common sources include Brazil, Uruguay, Mexico, India, and the western United States. Exact variety is uncertain from one image.
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