Georgbarsanovite is a rare member of the eudialyte group found primarily in the agpaitic alkaline massifs of the Kola Peninsula. It typically occurs as yellowish to brownish tabular crystals or massive grains within nepheline syenites and is highly prized by collectors for its complex chemical structure.
Is this georgbarsanovite?
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 georgbarsanovite with a known reference. Georgbarsanovite 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. Georgbarsanovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Georgbarsanovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive.
Often confused with
Georgbarsanovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside georgbarsanovite
Minerals reported to co-occur with georgbarsanovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₂Sr₄Ca₂Fe³⁺₃Zr₃NbSi₂₅O₇₃(O,OH,H₂O)₃(Cl,OH)₂
- Mohs hardness
- 5-6
- Density
- 2.98 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 Alkaline Igneous Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find georgbarsanovite
Classic worldwide localities
- Khibiny Massif, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in agpaitic alkaline igneous rocks country — that is the host setting where georgbarsanovite typically forms. If you start seeing nepheline, aegirine, microcline 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.






