Rock Identifier
Polished banded agate (likely purple chalcedony/jasper) (Microcrystalline quartz, SiO₂; chalcedony with iron-oxide-rich jasper bands) — mineral
mineral

Polished banded agate (likely purple chalcedony/jasper)

Microcrystalline quartz, SiO₂; chalcedony with iron-oxide-rich jasper bands

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; translucent purple, reddish-brown, and gray bands; vitreous to waxy luster; cryptocrystalline quartz with no cleavage; specific gravity about 2.6. The rough outer rind and polished face are characteristic of a cut slab or display specimen.

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Physical properties

Hardness 6.5–7 Mohs; translucent purple, reddish-brown, and gray bands; vitreous to waxy luster; cryptocrystalline quartz with no cleavage; specific gravity about 2.6. The rough outer rind and polished face are characteristic of a cut slab or display specimen.

Formation & geological history

Forms when silica-rich groundwater fills cavities in volcanic rock, depositing successive layers of chalcedony and jasper, commonly with iron staining. Individual agate bands may form over thousands to millions of years; the exact geological age is locality-dependent.

Uses & applications

Used for cabochons, carvings, bookends, decorative slabs, and lapidary objects; valued mainly for attractive banding and translucency.

Geological facts

Purple coloration may result from manganese, iron, or heat treatment, while reddish-brown zones commonly contain hematite or other iron oxides.

Field identification & locations

Identify by curved or parallel concentric banding, waxy quartz appearance, hardness, and inability to scratch with a steel knife easily. Common sources include Brazil, Uruguay, Mexico, Madagascar, and the western United States.