Kostylevite is a rare zirconium silicate mineral discovered in the alkaline massifs of the Kola Peninsula. It typically occurs as small, colorless prismatic crystals found within pegmatite veins associated with eudialyte-group minerals.
Is this kostylevite?
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 kostylevite with a known reference. Kostylevite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kostylevite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kostylevite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial aggregates.
Often confused with
Kostylevite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kostylevite
Minerals reported to co-occur with kostylevite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₄Zr₂Si₆O₁₈·2H₂O
- Mohs hardness
- 5
- Density
- 2.74 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Radial Aggregates
- Cleavage
- {110}; {100}, Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
Where rockhounds find kostylevite
Classic worldwide localities
- Khibiny Massif (Russia)
- Lovozero Massif (Russia)
Field-hunting tip
Look in alkaline pegmatites country, the host setting where kostylevite typically forms. If you start seeing eudialyte, aegirine, nepheline in float, you are in the right ground. Field specimens usually show a prismatic crystals, radial aggregates habit, so train your eye for that shape before scanning the outcrop.






