
mineral
Banded agate beads
Agate, a microcrystalline variety of quartz (SiO₂)
AI-generated identification · may be incorrectGreen-and-white banded, polished beads with a waxy-to-glassy luster; Mohs hardness 6.5–7, trigonal quartz structure, no prominent cleavage, specific gravity about 2.6. The color may be enhanced by dyeing.
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Physical properties
Green-and-white banded, polished beads with a waxy-to-glassy luster; Mohs hardness 6.5–7, trigonal quartz structure, no prominent cleavage, specific gravity about 2.6. The color may be enhanced by dyeing.
Formation & geological history
Agate forms as silica-rich fluids deposit fine quartz and chalcedony in cavities, commonly in volcanic rocks; deposits span many geological ages. The beads are cut and polished from natural agate, though the image cannot establish whether the green color is natural.
Uses & applications
Used in jewelry and ornamental objects; attractive banding makes agate popular for beads and carvings.
Geological facts
Agate’s curved or parallel bands record successive silica deposits, and its microscopic quartz crystals give it a tough, compact texture.
Field identification & locations
Look for distinct bands and a hard, smooth surface; common sources include Brazil, Uruguay, India, and Madagascar. These appear to be shaped beads rather than a raw field specimen.
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