Irtyshite is an extremely rare tantalum-titanium mineral originally discovered in the Altai Mountains. It typically occurs as small, transparent tabular crystals associated with pegmatite minerals like albite and muscovite. Due to its extreme rarity, it is almost exclusively held by advanced scientific collections or specialized mineral enthusiasts.
Is this irtyshite?
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 irtyshite with a known reference. Irtyshite 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. Irtyshite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Irtyshite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals.
Often found alongside irtyshite
Minerals reported to co-occur with irtyshite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ta₂Ti₂O₁₀
- Mohs hardness
- 5-6
- Density
- 4.46 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- very expensive, strictly for advanced mineral collectors
Where rockhounds find irtyshite
Classic worldwide localities
- Irtysh River, Altai Mountains, Kazakhstan
Field-hunting tip
Look in granite pegmatites country — that is the host setting where irtyshite typically forms. If you start seeing albite, microcline, quartz 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.




