Zinnwaldite is a lithium-bearing mica that commonly occurs as short, thick tabular crystals or micaceous books. It is most often found in greisens and lithium-rich granite pegmatites, frequently associated with tin and tungsten deposits.
Is this zinnwaldite?
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 zinnwaldite with a known reference. Zinnwaldite sits at Mohs 2.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, pearly on cleavage.
- 4Match the color rangeCompare against the expected color range: light brown, silvery white, gray, yellowish white, greenish white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: micaceous, platy, pseudo hexagonal.
Often confused with
Zinnwaldite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads vitreous, pearly on cleavage on Zinnwaldite and splendent to submetallic, vitreous, pearly on cleavage on Biotite.

How to tell apart: Luster reads vitreous, pearly on cleavage on Zinnwaldite and pearly to vitreous on Lepidolite.

Often found alongside zinnwaldite
Minerals reported to co-occur with zinnwaldite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KLiFeAl(AlSi₃)O₁₀(F,OH)₂
- Mohs hardness
- 2.5-4
- Density
- 2.90-3.02 g/cm³
- Streak
- White
- Luster
- Vitreous, pearly on cleavage
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Micaceous, platy, pseudo hexagonal
- Cleavage
- {001}, perfect
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- In tin-bearing pneumatolytic deposits in greisen; more rarely in granites, granite pegmatites, and high-temperature quartz veins
Where rockhounds find zinnwaldite
1 mapped spotsClassic worldwide localities
- Amelia, Amelia Co., Virginia, USA
- Pala district, San Diego Co., and Crestmore, Riverside Co., California, USA
- Black Hills, around Keystone, Pennington Co., South Dakota, USA
- York district, Seward Peninsula, Alaska, USA
- Altenberg, Saxony, and Waldstein, Bavaria, Germany
- Tördal, Norway
Field-hunting tip
Where it forms: In tin-bearing pneumatolytic deposits in greisen; more rarely in granites, granite pegmatites, and high-temperature quartz veins. If you start seeing topaz, cassiterite, wolframite in float, you are in the right ground. Typical habit: micaceous, platy, pseudo hexagonal. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Wisconsin. Start trip planning there.





