Rock Identifier
Polished agate (likely chalcedony) (Microcrystalline quartz, SiO₂; agate is banded chalcedony) — mineral
mineral

Polished agate (likely chalcedony)

Microcrystalline quartz, SiO₂; agate is banded chalcedony

AI-generated identification · may be incorrect

Translucent brown-green polished stone with a waxy to vitreous luster; quartz crystal structure, Mohs hardness 6.5–7, no cleavage, specific gravity about 2.6. The image does not show enough detail to confirm agate banding or identify any treatment.

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Physical properties

Translucent brown-green polished stone with a waxy to vitreous luster; quartz crystal structure, Mohs hardness 6.5–7, no cleavage, specific gravity about 2.6. The image does not show enough detail to confirm agate banding or identify any treatment.

Formation & geological history

Chalcedony forms as silica precipitates in cavities and fractures, commonly in volcanic rocks; agate deposits span many geological ages. Its exact age and locality cannot be determined from the image.

Uses & applications

Used for cabochons, jewelry, ornaments, and decorative objects; agate is also used for small precision components.

Geological facts

Agate is a variety of chalcedony, not a separate mineral species; distinctive curved or concentric bands are common but not visible here.

Field identification & locations

Look for translucent edges, fine banding, and hardness sufficient to scratch glass; common sources include Brazil, Uruguay, India, and the western United States. A locality or reliable identification requires closer examination.