Torreyite is a rare secondary mineral typically found as small, yellow, platy or radiating crystals. It is most famous from the zinc mines of Franklin and Sterling Hill, New Jersey, where it forms in oxidized zones of ore bodies.
Is this torreyite?
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 torreyite with a known reference. Torreyite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Torreyite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Torreyite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, radial aggregates, crusts.
Often confused with
Torreyite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside torreyite
Minerals reported to co-occur with torreyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Mn,Zn)₁₅(SO₄)₂(OH)₂₂·8H₂O
- Mohs hardness
- 2-3
- Density
- 2.84 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Radial Aggregates, Crusts
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Zinc Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find torreyite
Classic worldwide localities
- Sterling Hill Mine, New Jersey, USA
- Franklin Mine, New Jersey, USA
- Långban, Sweden
Field-hunting tip
Look in metamorphosed zinc ore deposits country — that is the host setting where torreyite typically forms. If you start seeing zincite, willemite, franklinite in float, you are in the right ground. Field specimens usually show a platy crystals, radial aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.






