Parabrandtite is a rare manganese arsenate mineral found primarily in the unique deposit at the Sterling Hill Mine. It typically forms colorless to white, thin bladed crystals and is visually difficult to distinguish from its polymorph, Brandtite, without laboratory analysis.
Is this parabrandtite?
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 parabrandtite with a known reference. Parabrandtite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: aggregates.
Often confused with
Parabrandtite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside parabrandtite
Minerals reported to co-occur with parabrandtite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Mn(AsO₄)₂·2H₂O
- Mohs hardness
- 3-4
- Density
- 3.55 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Aggregates
- Cleavage
- On {010} and {110}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Very rare, in a vein in primary ore from a metamorphosed stratiform zinc orebody
Where rockhounds find parabrandtite
Classic worldwide localities
- Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: Very rare, in a vein in primary ore from a metamorphosed stratiform zinc orebody. If you start seeing sarkinite, franklinite, willemite in float, you are in the right ground. Typical habit: aggregates. Train your eye for that shape before scanning the outcrop.






