Tiettaite is a rare potassium sodium iron silicate, typically grayish white. It occurs in unweathered ultra-alkalic pegmatites in an alkalic massif. It was first described from Mts. Koashva and Rasvumchorr, Khibiny massif, Kola Peninsula, Russia.
Is this tiettaite?
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 tiettaite with a known reference. Tiettaite 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 or silky.
- 4Match the color rangeCompare against the expected color range: grayish white, colorless, dark gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: aggregates.
Often confused with
Tiettaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tiettaite
Minerals reported to co-occur with tiettaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₄Na₁₂Fe³⁺₂Si₁₆O₄₁(OH)₄·2H₂O
- Mohs hardness
- 3
- Density
- 2.42 g/cm³
- Streak
- White
- Luster
- Vitreous or silky
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Aggregates
- Cleavage
- On {100} and {010}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In unweathered ultra-alkalic pegmatites in an alkalic massif
Where rockhounds find tiettaite
Classic worldwide localities
- Mts. Koashva and Rasvumchorr, Khibiny massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In unweathered ultra-alkalic pegmatites in an alkalic massif. If you start seeing nepheline, orthoclase, sodalite in float, you are in the right ground. Typical habit: aggregates. Train your eye for that shape before scanning the outcrop.







