Thomsenolite is a rare fluoride mineral often found as an alteration product of cryolite in pegmatitic environments. It is best identified by its prismatic to pseudo-octahedral habits and its distinct association with the Greenland cryolite deposit.
Is this thomsenolite?
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 thomsenolite with a known reference. Thomsenolite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Thomsenolite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Thomsenolite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Thomsenolite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside thomsenolite
Minerals reported to co-occur with thomsenolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCaAlF₆·H₂O
- Mohs hardness
- 2
- Density
- 2.95-3.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Massive, Granular
- Cleavage
- Good in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Cryolite-bearing Pegmatites
- Typical price
- $20-200 depending on specimen quality
Where rockhounds find thomsenolite
Classic worldwide localities
- Ivittuut, Greenland
- St. Peters Dome, USA
- Miass, Russia
Field-hunting tip
Look in cryolite-bearing pegmatites country — that is the host setting where thomsenolite typically forms. If you start seeing cryolite, pachnolite, siderite in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.




