
Mineral
Fuchsite
Chromium-rich Muscovite (K(Al,Cr)2(AlSi3O10)(OH)2)
Hardness: 2-2.5 (Mohs scale), Color: Emerald-green to light green, Luster: Vitreous to pearly, Crystal structure: Monoclinic, Cleavage: Perfect basal, Specific Gravity: 2.8-2.9.
- Hardness
- 2-2
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Physical properties
Hardness: 2-2.5 (Mohs scale), Color: Emerald-green to light green, Luster: Vitreous to pearly, Crystal structure: Monoclinic, Cleavage: Perfect basal, Specific Gravity: 2.8-2.9.
Formation & geological history
Metamorphic formation found primarily in phyllites and schists where chromium-bearing fluids interact with mica during regional metamorphism. Common in Precambrian greenstone belts.
Uses & applications
Used primarily as decorative stone, in lapidary work for cabochons, as a source for green pigment, and occasionally as a minor ore of chromium. Popular among metaphysical collectors.
Geological facts
Fuchsite is named after the German chemist Johann Nepomuk von Fuchs. It is a chrome-bearing variety of muscovite, where chromium replaces aluminum in the crystal lattice to give its distinctive green hue.
Field identification & locations
Identify in the field by its mica-like flaky habit, emerald green color, and softness (can be scratched by a fingernail). Commonly found in Brazil, India, Russia, and the Alps.
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