Nifontovite is a rare calcium borate mineral typically found in complex skarn environments. It is most easily identified by its colorless to white prismatic or tabular crystal habits, often occurring as delicate clusters within host rocks like charoite or limestone.
Is this nifontovite?
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 nifontovite with a known reference. Nifontovite sits at Mohs 3.5-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to silky.
- 4Match the color rangeCompare against the expected color range: colorless, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, radiating aggregates, massive.
Often confused with
Nifontovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nifontovite
Minerals reported to co-occur with nifontovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃[BO(OH)₂]₆(H₂O)₂
- Mohs hardness
- 3.5-5
- Density
- 2.35-2.36 g/cm³
- Streak
- White
- Luster
- Vitreous to silky
- Transparency
- Semitransparent to transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, radiating aggregates, massive
- Cleavage
- One, || elongation, poor
- Fluorescence
- Violet under LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a skarn formed by quartz diorite intruding limestone (Novofrolovo mine, Russia); near gehlenite-spurrite skarn formed by hydrothermal alteration (Fuka, Japan)
Where rockhounds find nifontovite
Classic worldwide localities
- Novofrolovo mine, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, Russia
- Fuka, near Bicchu, Okayama Prefecture, Japan
- Charcas, San Luis Potosi, Mexico
Field-hunting tip
Where it forms: In a skarn formed by quartz diorite intruding limestone (Novofrolovo mine, Russia); near gehlenite-spurrite skarn formed by hydrothermal alteration (Fuka, Japan). If you start seeing grossular-andradite, szaibélyite, sibirskite in float, you are in the right ground. Typical habit: tabular crystals, radiating aggregates, massive. Train your eye for that shape before scanning the outcrop.









