Dickinsonite-(KMnNa) is a rare secondary phosphate mineral typically found in complex granite pegmatites. Collectors look for its characteristic olive-green, platy, or foliated habits that often form in cavities alongside other secondary phosphates.
Is this dickinsonite-(kmnna)?
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 dickinsonite-(kmnna) with a known reference. Dickinsonite-(KMnNa) sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dickinsonite-(KMnNa) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Dickinsonite-(KMnNa) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: olive-green, yellow-green, brownish-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, foliated masses, lamellar aggregates.
Often confused with
Dickinsonite-(KMnNa) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside dickinsonite-(kmnna)
Minerals reported to co-occur with dickinsonite-(kmnna). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KNa₄Mn₁₄Al(PO₄)₁₂(OH)₂
- Mohs hardness
- 3.5-4
- Density
- 3.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Foliated Masses, Lamellar Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find dickinsonite-(kmnna)
Classic worldwide localities
- Branchville, Connecticut, USA
- Poland, Maine, USA
- Hagendorf, Bavaria, Germany
- Tip Top mine, South Dakota, USA
Field-hunting tip
Look in granite pegmatites country — that is the host setting where dickinsonite-(kmnna) typically forms. If you start seeing eosphorite, triphylite, apatite in float, you are in the right ground. Field specimens usually show a tabular crystals, foliated masses, lamellar aggregates habit, so train your eye for that shape before scanning the outcrop.






