Rock Identifier
Fuchsite (Chromium-rich Muscovite (K(Al,Cr)2(AlSi3O10)(OH)2)) — mineral
mineral

Fuchsite

Chromium-rich Muscovite (K(Al,Cr)2(AlSi3O10)(OH)2)

Hardness: 2-3 (Mohs scale), Color: Emerald green to light green, Luster: Pearly to vitreous, Crystal Structure: Monoclinic (usually micaceous/flaky), Cleavage: Perfect basal, Specific Gravity: 2.8-3.0

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Physical properties

Hardness: 2-3 (Mohs scale), Color: Emerald green to light green, Luster: Pearly to vitreous, Crystal Structure: Monoclinic (usually micaceous/flaky), Cleavage: Perfect basal, Specific Gravity: 2.8-3.0

Formation & geological history

Formed through regional metamorphism. The green color is derived from chromium trivalent ions replacing aluminum in the crystal structure of muscovite. Commonly found in phyllites and schists.

Uses & applications

Metaphysical and ornamental use, minor source of chromium, and used in crushed forms for glittery aesthetic effects in crafts.

Geological facts

Fuchsite is named after the German chemist Johann Nepomuk von Fuchs. It is essentially a green variety of mica. When it occurs with ruby inclusions, it is the popular gemstone known as Ruby in Fuchsite.

Field identification & locations

Identified by its signature green color combined with a flaky, mica-like texture that sparkles (micaceous). Commonly found in Brazil, India, and Russia. Collectors look for high luster and deep green saturation.