Låvenite is a rare zirconium-rich silicate mineral primarily found in silica-undersaturated alkaline pegmatites. It is typically identified by its prismatic, yellowish to brownish crystals and its association with other rare zirconium and titanium minerals in complex igneous environments.
Is this låvenite?
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 låvenite with a known reference. Låvenite 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. Låvenite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Låvenite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, sometimes tabular or fibrous.
Often confused with
Låvenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside låvenite
Minerals reported to co-occur with låvenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₂(Mn,Fe²⁺)(Zr,Ti,Nb)Si₂O₈(O,OH,F)₂
- Mohs hardness
- 6
- Density
- 3.5-3.6 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Sometimes Tabular or Fibrous
- Cleavage
- Distinct On {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites and Alkaline Igneous Rocks
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find låvenite
Classic worldwide localities
- Låven, Langesundsfjord, Norway
- Khibiny Massif, Russia
- Mont Saint-Hilaire, Canada
- Narssârssuk, Greenland
Field-hunting tip
Look in nepheline syenite pegmatites and alkaline igneous rocks country — that is the host setting where låvenite typically forms. If you start seeing nepheline, aegirine, eudialyte in float, you are in the right ground. Field specimens usually show a prismatic crystals, sometimes tabular or fibrous habit, so train your eye for that shape before scanning the outcrop.






