Petalite is a lithium-rich silicate mineral primarily found in lithium-bearing pegmatites. It is sought after by collectors for its transparent, gem-quality crystals, though it is often brittle and requires care when handled or faceted.
Is this petalite?
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 petalite with a known reference. Petalite sits at Mohs 6-6.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Petalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Petalite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray, yellow, pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, columnar.
Often confused with
Petalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside petalite
Minerals reported to co-occur with petalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- LiAlSi₄O₁₀
- Mohs hardness
- 6-6.5
- Density
- 2.3-2.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Columnar
- Cleavage
- Perfect Basal
- Fluorescence
- Occasionally Orange or Blue Under UV
- Rarity
- Uncommon
- Uses
- Gemstone, Collector, Industrial Source of Lithium
- Host rock
- Granite Pegmatites
- Typical price
- $10-50 per gram for gem quality
Where rockhounds find petalite
Classic worldwide localities
- Uto, Sweden
- Bikita, Zimbabwe
- Tanco Mine, Canada
- Karibib, Namibia
- Newry, Maine, USA
Field-hunting tip
Look in granite pegmatites country — that is the host setting where petalite typically forms. If you start seeing spodumene, lepidolite, tourmaline in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, columnar habit, so train your eye for that shape before scanning the outcrop.






