Polylithionite is a lithium-rich mica typically found in silica-undersaturated alkaline rocks and pegmatites. It often forms thin, platy, or tabular crystals that exhibit the classic perfect basal cleavage of the mica group, though it is usually identified by its association with rare alkaline minerals like Eudialyte.
Is this polylithionite?
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 polylithionite with a known reference. Polylithionite 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. Polylithionite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Polylithionite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale pink, pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, micaceous sheets, scaly aggregates.
Often confused with
Polylithionite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside polylithionite
Minerals reported to co-occur with polylithionite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KLi₂AlSi₄O₁₀(F,OH)₂
- Mohs hardness
- 2.5-3
- Density
- 2.8-2.9 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Micaceous Sheets, Scaly Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Alkaline Igneous Rocks, Pegmatites
- Typical price
- $10-60 per specimen
Where rockhounds find polylithionite
Classic worldwide localities
- Narsarsuk, Greenland
- Mont Saint-Hilaire, Canada
- Kola Peninsula, Russia
- Kvanefjeld, Greenland
Field-hunting tip
Look in alkaline igneous rocks, pegmatites country — that is the host setting where polylithionite typically forms. If you start seeing aegirine, microcline, sodalite in float, you are in the right ground. Field specimens usually show a tabular crystals, micaceous sheets, scaly aggregates habit, so train your eye for that shape before scanning the outcrop.








