Barentsite is a rare sodium aluminum carbonate-fluoride mineral typically found in hyperagpaitic pegmatites. Collectors should look for small, glassy, tabular crystals associated with bright red villiaumite or other alkaline minerals in the Kola Peninsula.
Is this barentsite?
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 barentsite with a known reference. Barentsite 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, pearly on cleavages; dull when altered.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: anhedral grains.
Often confused with
Barentsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside barentsite
Minerals reported to co-occur with barentsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₇Al(CO₃)₂(HCO₃)₂F₄
- Mohs hardness
- 3
- Density
- 2.56 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, pearly on cleavages; dull when altered
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Anhedral grains
- Cleavage
- {001} and {110}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Rare in hydrothermal veinlets in alkalic pegmatites in a differentiated alkalic massif
Where rockhounds find barentsite
Classic worldwide localities
- Mt. Restin’yun, Khibiny massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: Rare in hydrothermal veinlets in alkalic pegmatites in a differentiated alkalic massif. If you start seeing shortite, villiaumite, cryolite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.








