
gemstone
Polished dendritic agate (likely moss agate)
Microcrystalline quartz, SiO₂, with iron/manganese oxide inclusions
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent gray-brown body with darker branching or cloudlike inclusions, vitreous/waxy luster, cryptocrystalline structure, and no visible cleavage. The smoothly rounded surface indicates tumbling and polishing.
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Physical properties
Hardness 6.5–7 Mohs; translucent gray-brown body with darker branching or cloudlike inclusions, vitreous/waxy luster, cryptocrystalline structure, and no visible cleavage. The smoothly rounded surface indicates tumbling and polishing.
Formation & geological history
Forms when silica-rich groundwater fills cavities in volcanic rocks, depositing chalcedony and quartz in layers; metallic oxides create the dendritic patterns. It commonly formed during Cenozoic to older volcanic episodes, depending on locality.
Uses & applications
Used for cabochons, beads, carvings, paperweights, and decorative objects; generally an affordable lapidary material.
Geological facts
Despite its plantlike patterns, dendritic agate contains mineral inclusions rather than fossils or actual vegetation. Color and pattern arise mainly from iron and manganese oxides.
Field identification & locations
Identify it by its waxy translucence, conchoidal fracture, fine banding or dendrites, and glass-scratching hardness; common sources include Brazil, India, Madagascar, Uruguay, and the United States. A loupe may reveal curved growth bands and inclusions.
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