
gemstone
Polished moss agate (likely dendritic/mossy chalcedony)
Cryptocrystalline quartz, SiO₂, with green chlorite/iron-manganese inclusions
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent gray-green to creamy body with branching moss-like inclusions; vitreous to waxy luster, no visible cleavage, microcrystalline quartz structure, and specific gravity about 2.60–2.65.
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Physical properties
Hardness 6.5–7 Mohs; translucent gray-green to creamy body with branching moss-like inclusions; vitreous to waxy luster, no visible cleavage, microcrystalline quartz structure, and specific gravity about 2.60–2.65.
Formation & geological history
Forms when silica-rich groundwater fills cavities or fractures, trapping chlorite, hornblende, or manganese-oxide inclusions that create the moss patterns. It commonly formed in volcanic rocks during ancient hydrothermal activity, typically from Paleozoic to Cenozoic settings.
Uses & applications
Used for cabochons, beads, carvings, and inexpensive jewelry; polished pieces are also collected for their scenic patterns.
Geological facts
Despite its name, moss agate is not true agate in every specimen because it often lacks distinct banding. Green inclusions can resemble miniature landscapes, branches, or submerged vegetation.
Field identification & locations
Identify it by its hardness, waxy-translucent chalcedony body, and non-geometric green inclusions; it should not fizz in dilute acid. Common sources include India, Brazil, Uruguay, the United States, and Australia.
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