Paratsepinite-Ba is a rare member of the complex labuntsovite group of minerals, typically found in alkaline igneous environments. It occurs as small, glassy prismatic crystals that are challenging to distinguish from other group members without analytical testing.
Is this paratsepinite-ba?
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 paratsepinite-ba with a known reference. Paratsepinite-Ba 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: brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, prismatic.
Often confused with
Paratsepinite-Ba vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paratsepinite-ba
Minerals reported to co-occur with paratsepinite-ba. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ba,K,Na)₂(Ti,Nb)₄(Si₄O₁₂)₂(OH,O)₄·5H₂O
- Mohs hardness
- 5
- Density
- 2.88 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, prismatic
- Cleavage
- Imperfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In cavities formed by hydrothermal alteration of alkaline pegmatite
Where rockhounds find paratsepinite-ba
Classic worldwide localities
- Mt. Lepkhe-Nelm, Lovozero alkaline massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In cavities formed by hydrothermal alteration of alkaline pegmatite. If you start seeing titanite, aegirine, eudialyte in float, you are in the right ground. Typical habit: aggregates, prismatic. Train your eye for that shape before scanning the outcrop.








