Tsepinite-Sr is a rare member of the labuntsovite group typically found in alkaline igneous pegmatites. It forms small, prismatic to acicular crystals often grouped in radial or fan-like aggregates, and is primarily sought by advanced mineral collectors of complex silicates.
Is this tsepinite-sr?
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 tsepinite-sr with a known reference. Tsepinite-Sr 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial aggregates.
Often confused with
Tsepinite-Sr vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tsepinite-sr
Minerals reported to co-occur with tsepinite-sr. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Sr,Ba,K)(Ti,Nb)₂Si₄O₁₂(OH,O)₂·3H₂O
- Mohs hardness
- 5
- Density
- 2.67 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, radial aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In cavities formed by hydrothermal alteration of nepheline-syenite pegmatite
Where rockhounds find tsepinite-sr
Classic worldwide localities
- Mt. Eveslogchorr and Mt. Khibinpakhkchorr, Khibiny alkaline massif, and Mt. Lepkhe-Nel'm, Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In cavities formed by hydrothermal alteration of nepheline-syenite pegmatite. If you start seeing microcline, albite, natrolite in float, you are in the right ground. Typical habit: prismatic crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.








