
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 incorrectHardness 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.
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