Wadeite is a rare zirconium silicate mineral primarily found in silica-undersaturated alkaline rocks. It is highly prized by collectors for its distinct hexagonal crystal habit and its characteristic bright blue fluorescence under short-wave ultraviolet light.
Is this wadeite?
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 wadeite with a known reference. Wadeite sits at Mohs 6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Wadeite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Wadeite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale pink, pale blue.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic or tabular crystals.
Often confused with
Wadeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside wadeite
Minerals reported to co-occur with wadeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂ZrSi₃O₉
- Mohs hardness
- 6
- Density
- 3.19 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic or Tabular Crystals
- Cleavage
- Poor On Basal Pinacoid
- Fluorescence
- Bright Blue Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks and Pegmatites
- Typical price
- $50-500 depending on crystal size and quality
Where rockhounds find wadeite
Classic worldwide localities
- Khibiny Massif, Russia
- Murun Massif, Russia
- Mont Saint-Hilaire, Canada
- Ilimaussaq Complex, Greenland
Field-hunting tip
Look in alkaline igneous rocks and pegmatites country — that is the host setting where wadeite typically forms. If you start seeing nepheline, aegirine, microcline in float, you are in the right ground. Field specimens usually show a prismatic or tabular crystals habit, so train your eye for that shape before scanning the outcrop.





