Tisinalite is a rare member of the eudialyte group typically found in agpaitic alkaline pegmatites. It is visually similar to other eudialyte-group minerals and usually requires analytical methods for definitive identification, appearing as small, distinct yellow to brownish crystals.
Is this tisinalite?
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 tisinalite with a known reference. Tisinalite 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. Tisinalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tisinalite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: equant to tabular crystals.
Often confused with
Tisinalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tisinalite
Minerals reported to co-occur with tisinalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₆(Mn,□)₃(Fe,Mn)ZrSi₁₂O₃₀(OH,O)₂·H₂O
- Mohs hardness
- 5-6
- Density
- 2.83 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Equant to Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Agpaitic Pegmatites and Alkaline Igneous Complexes
- Typical price
- $50-300 per specimen
Where rockhounds find tisinalite
Classic worldwide localities
- Khibiny Massif, Kola Peninsula, Russia
Field-hunting tip
Look in agpaitic pegmatites and alkaline igneous complexes country — that is the host setting where tisinalite typically forms. If you start seeing aegirine, nepheline, lomonosovite in float, you are in the right ground. Field specimens usually show a equant to tabular crystals habit, so train your eye for that shape before scanning the outcrop.







