Imandrite is a rare member of the eudialyte group primarily found in the agpaitic rocks of the Kola Peninsula. It is typically identified by its trigonal crystal structure and association with other rare alkaline minerals, often requiring geochemical testing to distinguish it from other eudialyte-group members.
Is this imandrite?
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 imandrite with a known reference. Imandrite 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. Imandrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Imandrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: red, brown, pink, yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Imandrite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside imandrite
Minerals reported to co-occur with imandrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₂Ca₆(Fe,Mn)₃Zr₃Si₂₅O₇₃(O,OH,H₂O)₅Cl₂
- Mohs hardness
- 5-6
- Density
- 2.8-3.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-500 depending on size and crystal quality
Where rockhounds find imandrite
Classic worldwide localities
- Kola Peninsula, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where imandrite typically forms. If you start seeing aegirine, nepheline, microcline in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






