Uduminelite is a very rare silicate mineral first identified within the kimberlite pipes of the Yakutia region in Russia. It typically presents as small, delicate fibrous or acicular aggregates associated with secondary mineralization in ultrabasic rocks.
Is this uduminelite?
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 uduminelite with a known reference. Uduminelite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Uduminelite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Uduminelite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, acicular, or crusts.
Often confused with
Uduminelite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside uduminelite
Minerals reported to co-occur with uduminelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Mg₂Al₂Si₄O₁₂·4H₂O
- Mohs hardness
- 3-4
- Density
- 2.7-2.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, Acicular, Or Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Kimberlite
- Typical price
- niche/rare, pricing varies significantly by sample size
Where rockhounds find uduminelite
Classic worldwide localities
- Udachnaya Pipe, Yakutia, Russia
Field-hunting tip
Look in kimberlite country — that is the host setting where uduminelite typically forms. If you start seeing calcite, serpentine, phlogopite in float, you are in the right ground. Field specimens usually show a fibrous, acicular, or crusts habit, so train your eye for that shape before scanning the outcrop.




