Parakuzmenkoite-Fe is a rare member of the complex labuntsovite group, typically found in agpaitic alkaline pegmatites. It occurs as small, brownish, prismatic crystals often nestled within cavities of host rocks. Identification usually requires X-ray diffraction or chemical analysis due to the similarity between other members of its complex mineral group.
Is this parakuzmenkoite-fe?
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 parakuzmenkoite-fe with a known reference. Parakuzmenkoite-Fe 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. Parakuzmenkoite-Fe leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Parakuzmenkoite-Fe typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, yellow-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Parakuzmenkoite-Fe vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside parakuzmenkoite-fe
Minerals reported to co-occur with parakuzmenkoite-fe. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Ba,Na,H₂O)₄(Fe,Mn,Ti,Nb)₂(Ti,Nb)₂(Si₄O₁₂)₂(O,OH)₄·nH₂O
- Mohs hardness
- 5
- Density
- 2.88 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find parakuzmenkoite-fe
Classic worldwide localities
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where parakuzmenkoite-fe typically forms. If you start seeing microcline, aegirine, arfvedsonite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





