
mineral
Tumbled moss agate
Chalcedony (microcrystalline quartz, SiO₂) with moss-like inclusions
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent milky-white to gray body with dark green, possibly brown iron/manganese-oxide inclusions; waxy to vitreous luster, cryptocrystalline structure, no cleavage, specific gravity about 2.60.
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Physical properties
Hardness 6.5–7 Mohs; translucent milky-white to gray body with dark green, possibly brown iron/manganese-oxide inclusions; waxy to vitreous luster, cryptocrystalline structure, no cleavage, specific gravity about 2.60.
Formation & geological history
Forms when silica-rich groundwater deposits chalcedony in cavities and fractures, trapping dendritic inclusions—commonly chlorite, hornblende, or iron oxides. The specimen is polished/tumbled; its exact geological age cannot be determined from the image.
Uses & applications
Used for cabochons, beads, carvings, ornamental objects, and inexpensive collector specimens; generally not used as a major construction stone.
Geological facts
Despite the name, moss agate is usually not true agate banding and contains no organic moss. Its patterns are mineral inclusions revealed by translucent chalcedony.
Field identification & locations
Identify by its waxy translucent quartz body, curved polish, and branching green inclusions; common sources include India, Brazil, Uruguay, the United States, and Central Europe. A scratch test should be avoided on polished pieces.
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