Rock Identifier
Likely tumbled brown agate (Microcrystalline quartz (SiO₂), a variety of chalcedony) — mineral
mineral

Likely tumbled brown agate

Microcrystalline quartz (SiO₂), a variety of chalcedony

AI-generated identification · may be incorrect

Small, polished dark-brown pebble with possible lighter banding; quartz hardness 6.5–7 Mohs, vitreous to waxy luster, and no visible cleavage. The image is not detailed enough to confirm banding or identify the exact variety.

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Physical properties

Small, polished dark-brown pebble with possible lighter banding; quartz hardness 6.5–7 Mohs, vitreous to waxy luster, and no visible cleavage. The image is not detailed enough to confirm banding or identify the exact variety.

Formation & geological history

Agate forms as silica-rich fluids fill cavities in volcanic rocks and deposit layers of chalcedony; deposits span many geological ages. This specimen appears mechanically tumbled and polished.

Uses & applications

Used for jewelry, beads, ornaments, and collecting; agate is also used for decorative objects and, historically, precision instruments.

Geological facts

Agate is valued for its layered patterns, which can reveal successive episodes of mineral deposition.

Field identification & locations

Look for translucency at thin edges and curved or parallel bands; hardness and appearance alone cannot confirm agate from this photo. Agates occur worldwide, notably in Brazil, Uruguay, India, and the United States.