Yusupovite is a rare member of the eudialyte group primarily found in the agpaitic pegmatites of the Lovozero Massif in Russia. It typically occurs as yellowish to brownish tabular crystals or massive aggregates within alkalic igneous rocks. It is highly sought after by advanced collectors of rare earth and zirconium-bearing silicates.
Is this yusupovite?
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 yusupovite with a known reference. Yusupovite 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. Yusupovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Yusupovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive.
Often confused with
Yusupovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside yusupovite
Minerals reported to co-occur with yusupovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₀.₅K₂Zr(Si₆O₁₅)(OH)·H₂O
- Mohs hardness
- 5-6
- Density
- 2.88 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Agpaitic Pegmatites in Alkalic Massifs
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find yusupovite
Classic worldwide localities
- Mount Alluaiv, Lovozero Massif, Russia
- Kola Peninsula, Russia
Field-hunting tip
Look in agpaitic pegmatites in alkalic massifs country — that is the host setting where yusupovite typically forms. If you start seeing microcline, aegirine, nepheline in float, you are in the right ground. Field specimens usually show a tabular crystals, massive habit, so train your eye for that shape before scanning the outcrop.






