Bonshtedtite is a rare phosphate-carbonate mineral discovered in alkaline rock complexes, specifically those of the Kola Peninsula. It typically occurs as small, colorless to pale yellow tabular crystals embedded in pegmatitic matrices, often associated with other rare alkaline minerals like sidorenkite.
Is this bonshtedtite?
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 bonshtedtite with a known reference. Bonshtedtite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bonshtedtite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bonshtedtite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals or crystalline aggregates.
Often confused with
Bonshtedtite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bonshtedtite
Minerals reported to co-occur with bonshtedtite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃Fe(PO₄)(CO₃)
- Mohs hardness
- 3
- Density
- 2.66 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals or Crystalline Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites and Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find bonshtedtite
Classic worldwide localities
- Khibiny Massif, Russia
- Kovdor Massif, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in alkaline pegmatites and hydrothermal veins country — that is the host setting where bonshtedtite typically forms. If you start seeing aegirine, nepheline, sidorenkite in float, you are in the right ground. Field specimens usually show a tabular crystals or crystalline aggregates habit, so train your eye for that shape before scanning the outcrop.





