Hydroxyferroroméite is a rare iron antimony hydroxide, typically yellow to yellow-brown. It occurs in powdery boxwork replacements after tetrahedrite in a siderite-quartz matrix (France). Associated minerals include hematite, goethite and chalcopyrite. It was first described from Correc d'en Llinassos, near Oms, Pyrénées-Orientales Department, France.
Is this hydroxyferroroméite?
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 hydroxyferroroméite with a known reference. Hydroxyferroroméite 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. Streak: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: earthy to vitreous.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals, massive, granular.
Often confused with
Hydroxyferroroméite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hydroxyferroroméite
Minerals reported to co-occur with hydroxyferroroméite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe²⁺₁.₅☐₀.₅)Sb⁵⁺₂O₆(OH)
- Mohs hardness
- ~3
- Density
- 5.0-5.5 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Earthy to vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals, massive, granular
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As powdery boxwork replacements after tetrahedrite in a siderite-quartz matrix (France)
Where rockhounds find hydroxyferroroméite
Classic worldwide localities
- Correc d’en Llinassos, near Oms, Pyrénées-Orientales Department, France; also at the Consols Mine (ABH Consols Mine; Australian Broken Hill Consols Mine), Broken Hill, New South Wales, Australia
Field-hunting tip
Where it forms: As powdery boxwork replacements after tetrahedrite in a siderite-quartz matrix (France). If you start seeing hematite, goethite, chalcopyrite in float, you are in the right ground. Typical habit: octahedral crystals, massive, granular. Train your eye for that shape before scanning the outcrop.







