Reddingite is a rare phosphate mineral typically found in phosphate-rich zones of granite pegmatites. It forms short, blocky, prismatic crystals or compact granular masses that are prized by advanced collectors of phosphate minerals.
Is this reddingite?
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 reddingite with a known reference. Reddingite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Reddingite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Reddingite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, brownish-pink, yellowish-white, brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: short prismatic crystals, granular masses.
Often confused with
Reddingite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside reddingite
Minerals reported to co-occur with reddingite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn²⁺₃(PO₄)₂·3H₂O
- Mohs hardness
- 3-3.5
- Density
- 3.1-3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Short Prismatic Crystals, Granular Masses
- Cleavage
- Distinct On {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $20-200 per specimen
Where rockhounds find reddingite
Classic worldwide localities
- Branchville, Connecticut, USA
- Poland, Maine, USA
- Hagendorf, Bavaria, Germany
- Rapid Creek, Yukon, Canada
Field-hunting tip
Look in granite pegmatites country — that is the host setting where reddingite typically forms. If you start seeing triphylite, eosphorite, dickinsonite in float, you are in the right ground. Field specimens usually show a short prismatic crystals, granular masses habit, so train your eye for that shape before scanning the outcrop.




