Rock Identifier
Tumbled purple agate (likely grape agate or amethystine chalcedony) (Microcrystalline quartz, SiO₂; purple coloration commonly from iron, manganese, or inclusions) — mineral
mineral

Tumbled purple agate (likely grape agate or amethystine chalcedony)

Microcrystalline quartz, SiO₂; purple coloration commonly from iron, manganese, or inclusions

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; translucent purple-gray with darker dendritic or brecciated patterns and a waxy-to-glassy luster. Quartz has trigonal crystal structure, but chalcedony is cryptocrystalline and lacks visible cleavage.

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Physical properties

Hardness 6.5–7 Mohs; translucent purple-gray with darker dendritic or brecciated patterns and a waxy-to-glassy luster. Quartz has trigonal crystal structure, but chalcedony is cryptocrystalline and lacks visible cleavage.

Formation & geological history

Forms when silica-rich groundwater fills cavities in volcanic rock, depositing layered chalcedony and quartz over time; the specimen was later cut and polished. Most examples formed in Cenozoic volcanic terrains, though exact age is locality-dependent.

Uses & applications

Used for cabochons, beads, carvings, ornaments, and lapidary collections; durable but generally not high-value jewelry material.

Geological facts

“Grape agate” is a trade name for botryoidal purple chalcedony, especially from Indonesia; the pictured smooth stone may instead be dyed or naturally purple agate.

Field identification & locations

Identify by its glassy/waxy polish, fine internal banding or mossy patterns, absence of cleavage, and ability to scratch glass. Common sources include Indonesia, Brazil, Uruguay, Mexico, and Madagascar.