Alluaudite is a phosphate mineral commonly found as an alteration product of triphylite in complex pegmatites. It typically occurs as yellowish to brownish granular or fibrous masses rather than well-defined crystals, making it a challenging but rewarding find for phosphate mineral enthusiasts.
Is this alluaudite?
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 alluaudite with a known reference. Alluaudite sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: dirty yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: yellow, brownish yellow, green, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, nodular, platy.
Often confused with
Alluaudite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside alluaudite
Minerals reported to co-occur with alluaudite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- □NaMnFe₂(PO₄)₃
- Mohs hardness
- 5-5.5
- Density
- 3.45 g/cm³
- Streak
- Dirty yellow
- Luster
- Vitreous to resinous
- Transparency
- Subtranslucent to opaque
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, nodular, platy
- Cleavage
- {010}, {110}, and {11̄0}, good
- Rarity
- Uncommon
- Uses
- Collector, Scientific research
- Host rock
- Very common in granite pegmatites, formed by sodium metasomatism of triphylite-lithiophilite, heterosite-purpurite, or ferrisicklerite; in phosphatic nodules in shales
Where rockhounds find alluaudite
Classic worldwide localities
- G.E. Smith mine, near Newport, Sullivan Co., New Hampshire, USA
- La Vilate quarry, near Chanteloube, Haute-Vienne, France
- Dolní Bory, near Velkého Meziřičí, Czech Republic
- Varuträsk pegmatite, Västerbotten, Sweden
- Tremearne pegmatite, Breage, Cornwall, England
- Rapid Creek, Yukon Territory, Canada
Field-hunting tip
Where it forms: Very common in granite pegmatites, formed by sodium metasomatism of triphylite-lithiophilite, heterosite-purpurite, or ferrisicklerite; in phosphatic nodules in shales. If you start seeing triphylite, arrojadite, satterlyite in float, you are in the right ground. Typical habit: fibrous, nodular, platy. Train your eye for that shape before scanning the outcrop.





