
mineral
Polished banded agate
Microcrystalline quartz (SiO₂), variety agate
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; glossy vitreous polish with brown and white bands. Trigonal quartz, cryptocrystalline and without visible cleavage; specific gravity about 2.6.
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Physical properties
Hardness 6.5–7 Mohs; glossy vitreous polish with brown and white bands. Trigonal quartz, cryptocrystalline and without visible cleavage; specific gravity about 2.6.
Formation & geological history
Silica-rich fluids deposited successive layers in cavities, commonly in volcanic rocks; agates formed across many geological ages. The specimen appears shaped and polished.
Uses & applications
Used for jewelry, beads, ornaments, and lapidary collecting.
Geological facts
Agate’s curved or irregular bands form as silica layers accumulate, often recording changes in the cavity’s fluids.
Field identification & locations
Look for hardness, waxy-to-glassy luster, and distinctive internal banding; common sources include Brazil, Uruguay, India, and the United States. The image’s small size and polish limit reliable identification of its exact variety.
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