Niobokupletskite is a rare member of the astrophyllite group, primarily distinguished by its high niobium content. It typically occurs as brown, platy or bladed crystals found within peralkaline syenites and pegmatites, often forming radiating clusters that resemble the related astrophyllite.
Is this niobokupletskite?
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 niobokupletskite with a known reference. Niobokupletskite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Niobokupletskite leaves a brown streak.
- 3Read the lusterHold the specimen under a strong light. Niobokupletskite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: brown, dark brown, reddish-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, radial aggregates.
Often confused with
Niobokupletskite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside niobokupletskite
Minerals reported to co-occur with niobokupletskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂NaMn₇(Nb,Ti)₂Si₈O₂₄(O,OH,F)₇
- Mohs hardness
- 3-4
- Density
- 3.3-3.4 g/cm³
- Streak
- Brown
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Radial Aggregates
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find niobokupletskite
Classic worldwide localities
- Lovozero Massif, Russia
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where niobokupletskite typically forms. If you start seeing aegirine, nepheline, microcline in float, you are in the right ground. Field specimens usually show a platy crystals, radial aggregates habit, so train your eye for that shape before scanning the outcrop.






