
mineral
Moss Agate
Chalcedony (Silicon Dioxide, SiO2) with inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Cream, tan, brown, and green with dendritic inclusions; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None
- Hardness
- 6
- Color
- Cream, tan, brown, and green with dendritic inclusions
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Cream, tan, brown, and green with dendritic inclusions; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None
Formation & geological history
Formed through the deposition of silica in volcanic rock cavities or sedimentary veins. The characteristic 'moss' patterns are caused by manganese or iron oxide inclusions. Found in various geological ages from Precambrian to recent.
Uses & applications
Primarily used for lapidary work, jewelry (cabochons), pocket stones, and decorative carvings like the tree shape shown.
Geological facts
Despite its name, it does not contain organic matter; the 'moss' is actually mineral dendrites. It is historically known as a 'gardener's stone' believed to help crops grow.
Field identification & locations
Identify by its translucent body combined with dark, branch-like or moss-like inclusions. Commonly found in India, Brazil, and the USA (Montana/Oregon). Collectors look for high translucency and distinct dendritic patterns.
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