Zincoberaunite is a rare secondary phosphate mineral found primarily in granitic pegmatites. It typically forms as delicate, radiating sprays or crusts of acicular pale gray to silvery white crystals associated with other phosphate minerals.
Is this zincoberaunite?
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 zincoberaunite with a known reference. Zincoberaunite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: silky.
- 3Match the color rangeCompare against the expected color range: pale gray, silvery white.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: radial aggregates of acicular crystals.
Often confused with
Zincoberaunite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zincoberaunite
Minerals reported to co-occur with zincoberaunite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnFe₅(PO₄)₄(OH)₅·6H₂O
- Mohs hardness
- 3.5-4
- Density
- 2.92 g/cm³
- Colors
- Luster
- Silky
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Radial aggregates of acicular crystals
- Cleavage
- {100}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a zoned phosphatic granitic pegmatite
Where rockhounds find zincoberaunite
Classic worldwide localities
- Cornelia Mine Open Cut, Hagendorf South pegmatite, Upper Palatinate, Bavaria, Germany
Field-hunting tip
Where it forms: In a zoned phosphatic granitic pegmatite. If you start seeing potassium feldspar, quartz, jungite in float, you are in the right ground. Typical habit: radial aggregates of acicular crystals. Train your eye for that shape before scanning the outcrop.








