Ferrolaueite is a rare phosphate mineral that occurs as a secondary alteration product in complex granite pegmatites. It is typically identified as small, brownish tabular crystals closely associated with other phosphate minerals, often requiring X-ray diffraction or chemical analysis for definitive field identification.
Is this ferrolaueite?
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 ferrolaueite with a known reference. Ferrolaueite 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: brownish yellow, light yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Ferrolaueite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ferrolaueite
Minerals reported to co-occur with ferrolaueite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeFe₂(PO₄)₂(OH)₂·8H₂O
- Mohs hardness
- 3
- Density
- 2.75 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Probably considerd to be ferroan laueite and not s separate species
Where rockhounds find ferrolaueite
Classic worldwide localities
- Hagendorf-Pleystein Pegmatite (Germany)
- Tip Top Mine (USA)
Field-hunting tip
Where it forms: Probably considerd to be ferroan laueite and not s separate species. If you start seeing triphylite, sicklerite, phosphosiderite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





