Lovozerite is a rare zirconium-titanium silicate that typically occurs as an alteration product of eudialyte in alkaline igneous complexes. It is usually found as brown to pinkish-red equant grains or granular aggregates embedded within nepheline syenite rocks.
Is this lovozerite?
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 lovozerite with a known reference. Lovozerite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, resinous to dull.
- 4Match the color rangeCompare against the expected color range: dark brown, reddish brown, black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: massive, microscopic crystals, pseudo cubic.
Often confused with
Lovozerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lovozerite
Minerals reported to co-occur with lovozerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃CaZrSi₆O₁₅(OH)₃
- Mohs hardness
- 5
- Density
- 2.38-2.71 g/cm³
- Streak
- Brown
- Luster
- Vitreous, resinous to dull
- Transparency
- Transparent to opaque
- Crystal system
- Trigonal
- Crystal habit
- Massive, microscopic crystals, pseudo cubic
- Cleavage
- Two directions, imperfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In nepheline syenites and associated pegmatites
Where rockhounds find lovozerite
Classic worldwide localities
- Lovozero and Khibiny massifs, Kola Peninsula, Russia
- Ilímaussaq southern intrusion, Greenland
- Mont Saint-Hilaire, Quebec, Canada
Field-hunting tip
Where it forms: In nepheline syenites and associated pegmatites. If you start seeing potassic feldspar, nepheline, aegirine in float, you are in the right ground. Typical habit: massive, microscopic crystals, pseudo cubic. Train your eye for that shape before scanning the outcrop.






