
sedimentary
Moss Agate
Agate (Silicon Dioxide, SiO2) with dendritic inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Clear or milky white with green, brown, or black inclusions; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Clear or milky white with green, brown, or black inclusions
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Clear or milky white with green, brown, or black inclusions; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
Formation & geological history
Formed through the deposition of silica in rock cavities (vesicles) or cracks. The 'moss' effect is created by dendritic inclusions of manganese or iron oxides that crystallize as the silica solidifies. It occurs in volcanic environments over millions of years.
Uses & applications
Used primarily in jewelry, cabochons, and ornamental carvings. It is a popular collector's stone and is often used in artisan wire-wrapped pendants like the one shown.
Geological facts
Despite its name, Moss Agate does not contain organic matter; the plant-like patterns are strictly mineral. It was historically called 'Mocha Stone' after the city of Mocha in Yemen.
Field identification & locations
Identify in the field by its semi-transparent body and branching, plume-like internal inclusions. It is commonly found in India, Brazil, Uruguay, and the western United States. To differentiate from other jaspers, check for areas of translucency when held to light.
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