Raslakite is a rare mineral belonging to the eudialyte group, primarily identified in alkaline rocks of the Kola Peninsula. It typically occurs as small, equant crystals and is most easily distinguished from similar eudialyte-group minerals through precise chemical or X-ray diffraction analysis.
Is this raslakite?
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 raslakite with a known reference. Raslakite sits at Mohs 5, 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.
- 4Match the color rangeCompare against the expected color range: brownish red.
- 5Look at form & habitCrystal system: trigonal. Typical habit: granular.
Often confused with
Raslakite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside raslakite
Minerals reported to co-occur with raslakite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₅Ca₃Fe₃(Na,Zr)₃Zr₃(Si,Nb)Si₂₅O₇₃(OH,H₂O)₃(Cl,OH)
- Mohs hardness
- 5
- Density
- 2.95 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In an agpaitic pegmatite in an alkaline igneous complex
Where rockhounds find raslakite
Classic worldwide localities
- Mt. Kedykverpakhk, Lovozero alkaline massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In an agpaitic pegmatite in an alkaline igneous complex. If you start seeing microcline, aegirine, nepheline in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.








