Rock Identifier
Green agate (likely dyed), used as jewelry beads (Microcrystalline quartz, SiO₂ (chalcedony; agate variety)) — gemstone
gemstone

Green agate (likely dyed), used as jewelry beads

Microcrystalline quartz, SiO₂ (chalcedony; agate variety)

AI-generated identification · may be incorrect

Likely polished, irregular green beads with a waxy-to-vitreous luster; quartz hardness 6.5–7, trigonal crystal structure, specific gravity about 2.6. The image does not show diagnostic banding, and the color may be enhanced by dye.

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Physical properties

Likely polished, irregular green beads with a waxy-to-vitreous luster; quartz hardness 6.5–7, trigonal crystal structure, specific gravity about 2.6. The image does not show diagnostic banding, and the color may be enhanced by dye.

Formation & geological history

Agate forms as silica-rich fluids fill cavities in volcanic rock and deposit concentric or layered chalcedony over time; deposits span many geological ages. Green beads may be dyed after cutting and polishing.

Uses & applications

Used in beads, pendants, and other jewelry; agate is also used for carvings and decorative objects.

Geological facts

Agate is a banded variety of chalcedony, though bands may be subtle or absent in small bead material.

Field identification & locations

Green color and bead shape alone cannot confirm agate; inspect for fine banding and, where appropriate, test hardness on an inconspicuous surface. Agate occurs worldwide, notably in Brazil, Uruguay, India, and the United States.