Fuchsite is a chromium-rich variety of muscovite characterized by its brilliant, emerald-green color. It typically forms as platy aggregates or micaceous masses and is often found associated with quartz or kyanite in metamorphic environments.
Is this fuchsite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch fuchsite with a known reference. Fuchsite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Fuchsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fuchsite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: emerald-green, bright-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, micaceous masses.
Often confused with
Fuchsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fuchsite
Minerals reported to co-occur with fuchsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K(Al,Cr)₂(AlSi₃O₁₀)(OH)₂
- Mohs hardness
- 2.5-3
- Density
- 2.8 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Micaceous Masses
- Cleavage
- Perfect Basal
- Rarity
- Common
- Uses
- Collector, Lapidary
- Host rock
- Metamorphic Rocks, Hydrothermal Veins
- Typical price
- $5-30 for palm stones or specimens
Where rockhounds find fuchsite
Classic worldwide localities
- Minas Gerais, Brazil
- Zambales, Philippines
- Kola Peninsula, Russia
- Western Australia, Australia
- California, USA
Field-hunting tip
Look in metamorphic rocks, hydrothermal veins country — that is the host setting where fuchsite typically forms. If you start seeing quartz, kyanite, corundum in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous masses habit, so train your eye for that shape before scanning the outcrop.







