Paraumbite is a rare potassium zirconium silicate mineral found primarily in the unique alkaline massifs of the Kola Peninsula. It typically appears as small, tabular colorless to yellow crystals embedded within nepheline syenite pegmatites. Collectors should look for it in association with other rare zirconium minerals in hyper-alkaline environments.
Is this paraumbite?
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 paraumbite with a known reference. Paraumbite sits at Mohs ~4.5, 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 cleavages.
- 4Match the color rangeCompare against the expected color range: colorless, white, light yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: pseudo hexagonal.
Often confused with
Paraumbite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paraumbite
Minerals reported to co-occur with paraumbite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₃Zr₂H(Si₃O₉)₂·3H₂O
- Mohs hardness
- ~4.5
- Density
- 2.59 g/cm³
- Streak
- White
- Luster
- Vitreous, pearly on cleavages
- Transparency
- Translucent to transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Pseudo hexagonal
- Cleavage
- {010}, perfect micaceous; {100} and {110}, less perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Replacing wadeite in a pegmatite in a differentiated alkalic massif (Khibiny massif, Russia); in altered pegmatite and sodalite xenoliths in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada)
Where rockhounds find paraumbite
Classic worldwide localities
- Mt. Eveslogchorr, Khibiny massif, Kola Peninsula, Russia
- Mont Saint-Hilaire, Quebec, Canada
Field-hunting tip
Where it forms: Replacing wadeite in a pegmatite in a differentiated alkalic massif (Khibiny massif, Russia); in altered pegmatite and sodalite xenoliths in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada). If you start seeing eudialyte, wadeite, gaidonnayite in float, you are in the right ground. Typical habit: pseudo hexagonal. Train your eye for that shape before scanning the outcrop.






