Fuchsite (Green Muscovite in Quartz)

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

Rock Type: metamorphic

Fuchsite (Green Muscovite in Quartz)

Physical Properties

Hardness: 2-3 (mica) though often 7 in quartz matrix; Color: Emerald green to light green; Luster: Pearly to vitreous; Crystal Structure: Monoclinic; Cleavage: Perfect basal; Specific Gravity: 2.8 - 2.9

Formation & Geological History

Formed through the regional metamorphism of rocks rich in chromium. It is a phyllosilicate mineral commonly found in schists and gneisses, often associated with hydrothermal activity in quartz veins.

Uses & Applications

Used primarily as decorative stone, in jewelry as cabochons or beads, and as a source of chromium. It is also a popular specimen for gemstone collectors and metaphysical practitioners.

Geological Facts

Fuchsite is named after the German chemist and mineralogist Johann Nepomuk von Fuchs. When tiny flakes of fuchsite are suspended in quartz, it creates the gemstone known as Green Aventurine.

Field Identification & Locations

Identify in the field by its distinct forest-to-emerald green color and micaceous sheen. It is common in areas with metamorphic activity such as Brazil, India, and parts of the United States like New Hampshire.

Identified on: 4/13/2026

Mode: Standard