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?
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 kumtyubeite with a known reference. Kumtyubeite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kumtyubeite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kumtyubeite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: light-pink, colorless.
- 5Look 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
- Ca₄(Si₂O₇)F₂
- Mohs hardness
- 5-6
- Density
- 3.17 g/cm³
- Colors
- Streak
- White
- 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
- Pyrometamorphic Rocks
Where rockhounds find kumtyubeite
Classic worldwide localities
- Kumtyube, Kabardino-Balkarian Republic, Russia
Field-hunting tip
Look in pyrometamorphic rocks country, the host setting where kumtyubeite typically forms. If you start seeing ettringite, portlandite, afwillite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





