Bussenite is a rare titanium-rich silicate mineral primarily found in alkaline intrusive complexes. Collectors should look for its characteristic yellowish-brown platy crystals or fibrous mats associated with nepheline-bearing pegmatites.
Is this bussenite?
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 bussenite with a known reference. Bussenite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bussenite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bussenite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, fibrous aggregates.
Often confused with
Bussenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bussenite
Minerals reported to co-occur with bussenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ba₂TiMnSi₄O₁₄(OH,F)₂
- Mohs hardness
- 3-4
- Density
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Fibrous Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find bussenite
Classic worldwide localities
- Kola Peninsula, Russia
- Mont Saint-Hilaire, Canada
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where bussenite typically forms. If you start seeing aegirine, nepheline, microcline in float, you are in the right ground. Field specimens usually show a platy crystals, fibrous aggregates habit, so train your eye for that shape before scanning the outcrop.





