Pieczkaite is a rare manganese-dominant member of the apatite group characterized by its distinct yellow to brownish prismatic crystals. It is primarily found in granite pegmatites and is highly sought after by mineral collectors due to its rarity and specific chemical composition.
Is this pieczkaite?
4-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 pieczkaite with a known reference. Pieczkaite sits at Mohs 4-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: grayish white.
- 3Match the color rangeCompare against the expected color range: gray.
- 4Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Pieczkaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pieczkaite
Minerals reported to co-occur with pieczkaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₅(PO₄)₃Cl
- Mohs hardness
- 4-5
- Density
- 3.783 g/cm³
- Colors
- Streak
- Grayish white
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As small patches and narrow veins in apatite and (Mn,Cl)-bearing apatite in phosphate pods in the interior wall zone of the quartz core of a granitic pegmatite
Where rockhounds find pieczkaite
Classic worldwide localities
- Pegmatite no. 22, southeastern shoreline of an unnamed island in Cross Lake, Manitoba, Canada
Field-hunting tip
Where it forms: As small patches and narrow veins in apatite and (Mn,Cl)-bearing apatite in phosphate pods in the interior wall zone of the quartz core of a granitic pegmatite. If you start seeing fluorapatite, manitobaite, eosphorite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.






