Pattersonite is a rare lead-iron sulfide that occurs as a rare local variation within basalt cavities. It is visually indistinguishable from massive galena to the naked eye and typically requires chemical analysis or X-ray diffraction for definitive identification.
Is this pattersonite?
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 pattersonite with a known reference. Pattersonite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pattersonite leaves a grey streak.
- 3Read the lusterHold the specimen under a strong light. Pattersonite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, silver-white.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, granular.
Often confused with
Pattersonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pattersonite
Minerals reported to co-occur with pattersonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Pb,Fe)S
- Mohs hardness
- 2.5-3
- Density
- 7.3-7.5 g/cm³
- Colors
- Streak
- Grey
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Granular
- Cleavage
- Perfect Cubic
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Basaltic Traps
- Typical price
- $50-300 per specimen
Where rockhounds find pattersonite
Classic worldwide localities
- Patterson, New Jersey, USA
Field-hunting tip
Look in basaltic traps country — that is the host setting where pattersonite typically forms. If you start seeing prehnite, datolite, calcite in float, you are in the right ground. Field specimens usually show a massive, granular habit, so train your eye for that shape before scanning the outcrop.





