Chivruaiite is a rare mineral from the Labuntsovite group typically found in the alkaline pegmatites of the Kola Peninsula. It usually appears as small, vibrant yellow to brownish-yellow prismatic crystals associated with other rare alkaline minerals.
Is this chivruaiite?
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 chivruaiite with a known reference. Chivruaiite sits at Mohs 3, 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: pale pink, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular, aggregates, radial.
Often confused with
Chivruaiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chivruaiite
Minerals reported to co-occur with chivruaiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄(Ti,Nb)₅(Si₆O₁₇)₂(OH,O)₅·13-14H₂O
- Mohs hardness
- 3
- Density
- 2.4-2.42 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular, aggregates, radial
- Cleavage
- Distinct on {100}; distinct on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Found in three different hydrothermal veins within the Khibiny and Lovozero alkaline massifs associated with microcline, eudialyte, natrolite, astrophyllite, aegirine, etc
Where rockhounds find chivruaiite
Classic worldwide localities
- Chivruai river valley, Lovozero massif, Kola Peninsula, Russia (type locality)
Field-hunting tip
Where it forms: Found in three different hydrothermal veins within the Khibiny and Lovozero alkaline massifs associated with microcline, eudialyte, natrolite, astrophyllite, aegirine, etc. If you start seeing eudialyte, microcline, aegirine in float, you are in the right ground. Typical habit: acicular, aggregates, radial. Train your eye for that shape before scanning the outcrop.






