Koashvite is a rare member of the eudialyte group found primarily in the agpaitic alkaline rocks of the Kola Peninsula. It typically occurs as reddish, tabular crystals embedded within pegmatitic zones of nepheline syenites. Collectors look for its characteristic trigonal symmetry and association with other rare-earth-bearing silicate minerals.
Is this koashvite?
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 koashvite with a known reference. Koashvite 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. Koashvite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Koashvite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: red, brownish-red, yellow-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Koashvite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside koashvite
Minerals reported to co-occur with koashvite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₆(Fe,Mn)(Zr,Ti)Si₆(O,OH,F)₁₈(Cl,OH)
- Mohs hardness
- 5-6
- Density
- 2.95-3.05 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Alkaline Pegmatites and Nepheline Syenites
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find koashvite
Classic worldwide localities
- Khibiny Massif (Kola Peninsula, Russia)
- Lovozero Massif (Kola Peninsula, Russia)
Field-hunting tip
Look in alkaline pegmatites and nepheline syenites country — that is the host setting where koashvite 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, granular habit, so train your eye for that shape before scanning the outcrop.






