Fluornatromicrolite is a rare member of the pyrochlore supergroup characterized by high sodium and fluorine content in its structure. It typically occurs as small, sharp octahedral crystals in rare alkaline igneous environments. Collectors should be aware of its inherent radioactivity due to common substitution of radioactive elements within the crystal lattice.
Is this fluornatromicrolite?
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 fluornatromicrolite with a known reference. Fluornatromicrolite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: green.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Fluornatromicrolite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fluornatromicrolite
Minerals reported to co-occur with fluornatromicrolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na₁.₅Bi₀.₅)Ta₂O₆F
- Mohs hardness
- 5
- Density
- 6.49 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a granitic pegmatite
Where rockhounds find fluornatromicrolite
Classic worldwide localities
- Alto Quixaba pegmatite, Frei Martinho municipality, Paraíba State, northeastern Brazil
- Altai Mounains, Russia and the Borborema pegmatitic province, northeastern Brazil
Field-hunting tip
Where it forms: In a granitic pegmatite. If you start seeing perthitic microcline, albite, amblygonite in float, you are in the right ground. Typical habit: octahedral crystals. Train your eye for that shape before scanning the outcrop.







