Gorbunovite is a rare titanium-niobium silicate mineral found primarily within the highly alkaline pegmatites of the Khibiny Massif. It typically occurs as small, yellow, platy crystals, requiring careful microscopic examination to distinguish it from related members of the Tundrite group.
Is this gorbunovite?
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 gorbunovite with a known reference. Gorbunovite sits at Mohs 3.5-4, 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: yellow, brownish yellow, orange.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals.
Often confused with
Gorbunovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gorbunovite
Minerals reported to co-occur with gorbunovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CsLi₂(Ti,Fe³⁺)Si₄O₁₀(F,OH,O)₂
- Mohs hardness
- 3.5-4
- Density
- 3.59 g/cm³
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- agpaitic pegmatites in alkaline complexes
Where rockhounds find gorbunovite
Classic worldwide localities
- Darai-Pioz glacier, Alai mountain range, Tien Shan, Rashtskiy (formerly Garmskiy) district, Tajikistan
Field-hunting tip
Where it forms: agpaitic pegmatites in alkaline complexes. If you start seeing nepheline, aegirine, microcline in float, you are in the right ground. Typical habit: platy crystals. Train your eye for that shape before scanning the outcrop.





