Byzantievite is a rare lead-titanium silicate mineral discovered in alkaline pegmatites of the Kola Peninsula. It typically occurs as small, brownish, platy crystals that exhibit perfect cleavage and are often found in complex associations with other rare-earth minerals.
Is this byzantievite?
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 byzantievite with a known reference. Byzantievite sits at Mohs 4.5-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to slightly greasy on fracture surfaces.
- 4Match the color rangeCompare against the expected color range: brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, granular aggregates.
Often confused with
Byzantievite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside byzantievite
Minerals reported to co-occur with byzantievite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba₅(Ca,REE,Y)₂₂(Ti,Nb)₁₈(SiO₄)₄(PO₄,SiO₄)₄(BO₃)₉O₂₂((OH),F)₄₃(H₂O)₁.₅
- Mohs hardness
- 4.5-5
- Density
- 4.10 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous to slightly greasy on fracture surfaces
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy crystals, granular aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a glacial moraine boulder of coarse-grained alkaline igneous rock
Where rockhounds find byzantievite
Classic worldwide localities
- Darai-Pioz alkaline massif, at the junction of the Turkestan, Zeravshan, and Alay Mountain Ranges, Tajikistan
Field-hunting tip
Where it forms: In a glacial moraine boulder of coarse-grained alkaline igneous rock. If you start seeing quartz, microcline, aegirine in float, you are in the right ground. Typical habit: platy crystals, granular aggregates. Train your eye for that shape before scanning the outcrop.







