
mineral
Fuchsite (Chrome Mica)
Chromian Muscovite - K(Al,Cr)2(AlSi3O10)(OH)2
Hardness: 2-2.5 on Mohs scale. Color: emerald green to yellowish-green due to chromium substitute. Luster: pearly to vitreous, highly micaceous and reflective. Cleavage: perfect in one direction, flaky. Crystal system: monoclinic.
- Hardness
- 2-2
- Color
- emerald green to yellowish-green due to chromium substitute
- Luster
- pearly to vitreous, highly micaceous and reflective
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Physical properties
Hardness: 2-2.5 on Mohs scale. Color: emerald green to yellowish-green due to chromium substitute. Luster: pearly to vitreous, highly micaceous and reflective. Cleavage: perfect in one direction, flaky. Crystal system: monoclinic.
Formation & geological history
Formed through regional metamorphism of rocks containing chromium, typically associated with mica schists, quartzites, and ultramafic rocks altered by hydrothermal activity.
Uses & applications
Popular as a decorative display mineral, gemstone material, and ornamental stone. Highly valued by collectors for its brilliant green shimmer and sparkle. Sometimes used in metaphysical carvings.
Geological facts
Fuchsite is named after the German chemist and mineralogist Johann Nepomuk von Fuchs. When fuchsite occurs as fine inclusions inside quartz, it creates the aventurescent gemstone known as Green Aventurine.
Field identification & locations
Identified in the field by its distinctive bright emerald-green color combined with typical mica features—flaky, flexible sheets that sparkle brilliantly in light. Commonly found in Brazil, Russia, Zimbabwe, Madagascar, and India.
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