Rock Identifier
Banded agate beads (Agate, a microcrystalline variety of quartz (SiO₂)) — mineral
mineral

Banded agate beads

Agate, a microcrystalline variety of quartz (SiO₂)

AI-generated identification · may be incorrect

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.

Identified More mineral →
Explore Banded agate beads in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

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.