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 3, 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: dull to silky.
- 4Match the color rangeCompare against the expected color range: white, light pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: spherical, tabular.
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)₂·3H₂O
- Mohs hardness
- 3
- Density
- 2.95 g/cm³
- Colors
- Streak
- White
- Luster
- Dull to silky
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Spherical, tabular
- Cleavage
- One, perfect, parallel to elongation
- Fluorescence
- Bright white under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A very rare mineral in seams in franklinite ore from a metamorphosed stratiform zinc orebody
Where rockhounds find sterlinghillite
Classic worldwide localities
- Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: A very rare mineral in seams in franklinite ore from a metamorphosed stratiform zinc orebody. If you start seeing franklinite, sphalerite, löllingite in float, you are in the right ground. Typical habit: spherical, tabular. Train your eye for that shape before scanning the outcrop.





