Robertsite is a rare phosphate mineral often found as pinkish, botryoidal or fibrous crusts within phosphate-rich pegmatites. Collectors primarily search for it in weathered phosphate zones where it forms as an alteration product of primary minerals like triphylite.
Is this robertsite?
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 robertsite with a known reference. Robertsite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Robertsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Robertsite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: pink, pale pink, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, crusts, or radiating fibrous aggregates.
Often confused with
Robertsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside robertsite
Minerals reported to co-occur with robertsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Mn₅(PO₄)₄(OH)₆·3H₂O
- Mohs hardness
- 3.5
- Density
- 3.2 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Crusts, Or Radiating Fibrous Aggregates
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate-rich Granite Pegmatites
- Typical price
- $20-150 thumbnail specimens
Where rockhounds find robertsite
Classic worldwide localities
- Tip Top mine (South Dakota, USA)
- Mangualde (Portugal)
- Hagendorf (Germany)
Field-hunting tip
Look in phosphate-rich granite pegmatites country — that is the host setting where robertsite typically forms. If you start seeing triphylite, ludlamite, hureaulite in float, you are in the right ground. Field specimens usually show a massive, crusts, or radiating fibrous aggregates habit, so train your eye for that shape before scanning the outcrop.






