Grischunite is a rare phosphate mineral originally discovered in the manganese deposits of the Falotta mine in Switzerland. It typically appears as reddish-brown massive or granular masses, making it a challenging mineral for field identification without specialized analytical methods.
Is this grischunite?
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 grischunite with a known reference. Grischunite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow-brown to orange.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: dark reddish brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular aggregates, rarely as small tabular crystals.
Often confused with
Grischunite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside grischunite
Minerals reported to co-occur with grischunite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂Mn₅Fe(AsO₄)₆·2H₂O
- Mohs hardness
- ~5
- Density
- 3.8 g/cm³
- Colors
- Streak
- Yellow-brown to orange
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Granular aggregates, rarely as small tabular crystals
- Cleavage
- On {010}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An alteration product of sarkinite in a manganese deposit
Where rockhounds find grischunite
Classic worldwide localities
- Falotta mine, Oberhalbstein, Graubünden, Switzerland
Field-hunting tip
Where it forms: An alteration product of sarkinite in a manganese deposit. If you start seeing sarkinite, brandtite, manganoan berzeliite in float, you are in the right ground. Typical habit: granular aggregates, rarely as small tabular crystals. Train your eye for that shape before scanning the outcrop.






