Sterlinghillite is an extremely rare manganese arsenate mineral known primarily from the famous Sterling Hill Mine. It usually occurs as microscopic, white to colorless platy crystals or crusts that are best identified by their characteristic bright white fluorescence under short-wave UV light.
Is this sterlinghillite?
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 sterlinghillite with a known reference. Sterlinghillite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sterlinghillite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sterlinghillite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Sterlinghillite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside sterlinghillite
Minerals reported to co-occur with sterlinghillite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₃(AsO₄)₂(OH)₂·4H₂O
- Mohs hardness
- 2
- Density
- 3.5 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts, Radial Aggregates
- Cleavage
- Perfect in One Direction
- Fluorescence
- Bright White Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Metamorphosed Zinc-manganese Ore Bodies
- Typical price
- $50-500 thumbnail depending on matrix and fluorescence quality
Where rockhounds find sterlinghillite
Classic worldwide localities
- Sterling Hill Mine, New Jersey, USA
Field-hunting tip
Look in hydrothermal veins in metamorphosed zinc-manganese ore bodies country — that is the host setting where sterlinghillite typically forms. If you start seeing willemite, franklinite, zincite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.




