![Fuchsite (Chromium-bearing Muscovite [K(Al,Cr)2(AlSi3O10)(OH)2]) — mineral](https://media.rockidentification.com/ec6b43c5-f3e4-4ac8-adb0-15c10e277f53-compressed.jpg)
mineral
Fuchsite
Chromium-bearing Muscovite [K(Al,Cr)2(AlSi3O10)(OH)2]
Hardness: 2-2.5 (Mohs scale); Color: Emerald green to light green; Luster: Pearly to vitreous; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific gravity: 2.80-2.88.
- Hardness
- 2-2
- Color
- Emerald green to light green
- Luster
- Pearly to vitreous
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Physical properties
Hardness: 2-2.5 (Mohs scale); Color: Emerald green to light green; Luster: Pearly to vitreous; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific gravity: 2.80-2.88.
Formation & geological history
Formed through regional metamorphism in phyllites and schists, particularly those rich in chromium. Found in rocks dating back to the Archean through Proterozoic eons.
Uses & applications
Used primarily as decorative stone, for carving figurines, in lapidary work (cabochons), and as a minor gemstone for collectors. Also used as a pigment or glitter source.
Geological facts
Fuchsite is named after the German chemist and mineralogist Johann Nepomuk von Fuchs. When mixed with large amounts of quartz, it forms a popular gemstone variety known as Green Aventurine.
Field identification & locations
Identify in the field by its distinctive green color, micaceous (sheet-like) habit, and low hardness (scratched by a fingernail). Common locations include Brazil, India, Zimbabwe, and Russia.
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