Manganoeudialyte is a manganese-rich member of the complex eudialyte group found in alkaline igneous environments. It is highly valued by collectors for its vibrant pink to magenta hues and often occurs as tabular crystals or massive grains within nepheline syenites.
Is this manganoeudialyte?
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 manganoeudialyte with a known reference. Manganoeudialyte 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. Manganoeudialyte leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Manganoeudialyte typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, red, magenta.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Manganoeudialyte vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside manganoeudialyte
Minerals reported to co-occur with manganoeudialyte. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₅Ca₆(Mn,Fe)₃Zr₃Si₂₆O₇₂Cl₂·H₂O
- 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
- Poor
- Rarity
- Rare
- Uses
- Collector, Geological Study
- Host rock
- Alkaline Igneous Rocks, Syenite Pegmatites
- Typical price
- $20-150 per specimen depending on size and intensity of color
Where rockhounds find manganoeudialyte
Classic worldwide localities
- Kola Peninsula, Russia
- Mont Saint-Hilaire, Canada
- Norra Kärr, Sweden
Field-hunting tip
Look in alkaline igneous rocks, syenite pegmatites country — that is the host setting where manganoeudialyte 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.






