Arrojadite-(PbFe) is a rare phosphate mineral primarily found in complex granite pegmatites. It usually occurs as massive, granular aggregates with a vitreous luster, appearing in shades of green or brown. Collectors often prize it as a significant species from lithium-bearing pegmatite localities.
Is this arrojadite-(pbfe)?
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 arrojadite-(pbfe) with a known reference. Arrojadite-(PbFe) sits at Mohs 3.5-4, 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: pale honey.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular.
Often confused with
Arrojadite-(PbFe) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside arrojadite-(pbfe)
Minerals reported to co-occur with arrojadite-(pbfe). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbFe²⁺(CaNa₂)Fe²⁺₁₃Al(PO₄)₁₁(PO₃OH)(OH)₂
- Mohs hardness
- 3.5-4
- Density
- 3.596 g/cm³
- Colors
- Pale honey
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Granular
- Cleavage
- On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A high-temperature (≈ 800°C) primary mineral in granite pegmatites
Where rockhounds find arrojadite-(pbfe)
Classic worldwide localities
- Sapucaia pegmatite, Galileia, Rio Doce basin, Minas Gerais, Brazil
Field-hunting tip
Where it forms: A high-temperature (≈ 800°C) primary mineral in granite pegmatites. If you start seeing triphylite, chloritized biotite, albite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.



