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, 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.





