Graftonite-(Mn) is a relatively rare phosphate mineral typically found in complex granite pegmatites. It is often distinguished by its distinct salmon-pink or brownish-red coloration and often occurs in intimate intergrowths with triphylite.
Is this graftonite-(mn)?
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-(mn) with a known reference. Graftonite-(Mn) 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-(Mn) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Graftonite-(Mn) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: salmon-pink, brownish-red, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Graftonite-(Mn) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside graftonite-(mn)
Minerals reported to co-occur with graftonite-(mn). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mn²⁺,Fe²⁺,Ca)₃(PO₄)₂
- Mohs hardness
- 5
- Density
- 3.67 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Good On {010}, Poor On {100}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Granite Pegmatites
- Typical price
- $20-150 for small specimens
Where rockhounds find graftonite-(mn)
Classic worldwide localities
- New Hampshire, USA
- Bavaria, Germany
- Norrö, Sweden
- Quebec, Canada
Field-hunting tip
Look in granite pegmatites country — that is the host setting where graftonite-(mn) typically forms. If you start seeing triphylite, albite, quartz in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







