Pararobertsite is a rare phosphate mineral typically found as microcrystalline crusts or powdery aggregates in granite pegmatites. It is often visually indistinguishable from its polymorph, robertsite, and usually requires X-ray diffraction for definitive identification.
Is this pararobertsite?
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 pararobertsite with a known reference. Pararobertsite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pararobertsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pararobertsite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: microcrystalline aggregates, crusts, powdery.
Often confused with
Pararobertsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pararobertsite
Minerals reported to co-occur with pararobertsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Mn₃(PO₄)₃(OH)₃·3H₂O
- Mohs hardness
- 3-4
- Density
- 3.37 g/cm³
- Colors
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Microcrystalline Aggregates, Crusts, Powdery
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate-rich Granite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find pararobertsite
Classic worldwide localities
- Tip Top mine, Custer, South Dakota, USA
- Mangualde, Portugal
Field-hunting tip
Look in phosphate-rich granite pegmatites country — that is the host setting where pararobertsite typically forms. If you start seeing robertsite, fairfieldite, triphylite in float, you are in the right ground. Field specimens usually show a microcrystalline aggregates, crusts, powdery habit, so train your eye for that shape before scanning the outcrop.




