Fluorcalcioroméite is a rare member of the pyrochlore supergroup typically found as small, sharp octahedral crystals in manganese-rich metamorphic rocks. It is highly prized by advanced mineral collectors for its distinct symmetry and association with unique mineral assemblages. Collectors should be aware of its toxic antimony content and maintain proper hygiene after physical contact.
Is this fluorcalcioroméite?
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 fluorcalcioroméite with a known reference. Fluorcalcioroméite 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: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: yellow, orange.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals, massive.
Often confused with
Fluorcalcioroméite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fluorcalcioroméite
Minerals reported to co-occur with fluorcalcioroméite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Na)₂Sb₂O₆F
- Mohs hardness
- ~5
- Density
- 5.113 g/cm³
- Streak
- White
- Luster
- Vitreous to resinous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals, massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a structurally deformed manganese deposit most likely of synsedimentary exhalative origin
Where rockhounds find fluorcalcioroméite
Classic worldwide localities
- Starlera mine, Ferrera, Hinterrhein district, Grischun, Switzerland
Field-hunting tip
Where it forms: In a structurally deformed manganese deposit most likely of synsedimentary exhalative origin. If you start seeing braunite, hematite, calcite in float, you are in the right ground. Typical habit: octahedral crystals, massive. Train your eye for that shape before scanning the outcrop.






