Graftonite-(Ca) is a rare phosphate mineral primarily found within zoned granitic pegmatites. It is typically identified by its flesh-colored to brownish appearance and its close association with triphylite, often forming intricate intergrowths that are fascinating for systematic mineral collectors.
Is this graftonite-(ca)?
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 graftonite-(ca) with a known reference. Graftonite-(Ca) sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Graftonite-(Ca) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Graftonite-(Ca) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pinkish-brown, brown, flesh-red.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: lamellar or granular masses.
Often confused with
Graftonite-(Ca) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside graftonite-(ca)
Minerals reported to co-occur with graftonite-(ca). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Fe²⁺,Mn²⁺)₃(PO₄)₂
- Mohs hardness
- 5
- Density
- 3.55-3.65 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Lamellar or Granular Masses
- Cleavage
- Distinct On {010}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Granite Pegmatites
- Typical price
- $20-100 for small study specimens
Where rockhounds find graftonite-(ca)
Classic worldwide localities
- Palermo Mine, New Hampshire, USA
- Norrö, Sweden
- Cross Lake, Manitoba, Canada
- Mangualde, Portugal
Field-hunting tip
Look in granite pegmatites country — that is the host setting where graftonite-(ca) typically forms. If you start seeing triphylite, apatite, muscovite in float, you are in the right ground. Field specimens usually show a lamellar or granular masses habit, so train your eye for that shape before scanning the outcrop.






