Kumtyubeite is a very rare calcium silicate fluoride mineral discovered in the pyrometamorphic rocks of the Northern Caucasus. It typically forms small tabular crystals within high-temperature combustion metamorphic assemblages and is highly prized by advanced mineral collectors.
Is this kumtyubeite?
4-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 kumtyubeite with a known reference. Kumtyubeite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: light-pink, colorless.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Kumtyubeite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kumtyubeite
Minerals reported to co-occur with kumtyubeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₅(SiO₄)₂F₂
- Mohs hardness
- 5-6
- Density
- 2.866 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals
- Cleavage
- Distinct on (001), particularly for OH:F ≈ 1
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rock-forming mineral in contact-metasomatic, spurrite-rondorfite-ellestadite skarn in carbonate-xenoliths in ignimbrites
Where rockhounds find kumtyubeite
Classic worldwide localities
- Kabardino-Balkaria, North Caucasus, Russia (type locality)
Field-hunting tip
Where it forms: A rock-forming mineral in contact-metasomatic, spurrite-rondorfite-ellestadite skarn in carbonate-xenoliths in ignimbrites. If you start seeing rondorfite, lakargiite, kimzeyite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





