Schmidite is a rare zinc iron manganese phosphate, typically orange-brown to copper-red. It occurs in and near altered phosphophyllite in a corroded triphylite nodule in granitic pegmatite. It was first described from Hagendorf-Süd pegmatite, Hagendorf, Oberpfalz, Bavaria, Germany.
Is this schmidite?
3-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 schmidite with a known reference. Schmidite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: orange-brown, copper-red.
- 3Look at form & habitCrystal system: orthorhombic. Typical habit: crusts, aggregates of tiny crystals.
Often confused with
Schmidite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside schmidite
Minerals reported to co-occur with schmidite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn(Fe³⁺₀.₅Mn²⁺₀.₅)₂ZnFe³⁺(PO₄)₃(OH)₃(H₂O)₈
- Mohs hardness
- 3
- Density
- 2.82 g/cm³
- Colors
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Crusts, aggregates of tiny crystals
- Cleavage
- Perfect on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On and near altered phosphophyllite in a corroded triphylite nodule in granitic pegmatite
Where rockhounds find schmidite
Classic worldwide localities
- Hagendorf-Süd pegmatite, Hagendorf, Oberpfalz, Bavaria, Germany
Field-hunting tip
Where it forms: On and near altered phosphophyllite in a corroded triphylite nodule in granitic pegmatite. If you start seeing phosphophyllite, vivianite, zwieselite in float, you are in the right ground. Typical habit: crusts, aggregates of tiny crystals. Train your eye for that shape before scanning the outcrop.







