Playfairite is a rare lead-antimony sulfosalt typically found as delicate, acicular, or lath-like metallic gray crystals. It is most notable for its occurrences in the Madoc area of Ontario, where it forms in hydrothermal environments. Collectors seek it for its structural complexity and rarity in the sulfosalt mineral group.
Is this playfairite?
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 playfairite with a known reference. Playfairite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: lead gray, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: striated, tabular.
Often confused with
Playfairite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Playfairite is noticeably harder (Mohs 3.5-4 vs. 2.5); streak differs, so Playfairite leaves black, Jamesonite leaves black. grayish.

How to tell apart: Playfairite is noticeably harder (Mohs 3.5-4 vs. 2); streak differs, so Playfairite leaves black, Stibnite leaves lead-gray.
Often found alongside playfairite
Minerals reported to co-occur with playfairite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₁₆(Sb,As)₁₉S₄₄Cl
- Mohs hardness
- 3.5-4
- Density
- 5.8 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Striated, tabular
- Cleavage
- {100}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As masses and stringers through dolomitic and calcitic marbles
Where rockhounds find playfairite
Classic worldwide localities
- Madoc, Ontario, Canada (type locality)
- Novoye, Khaydarkan, Fergana Valley, Alai Range, Kyrgyzstan
Field-hunting tip
Where it forms: As masses and stringers through dolomitic and calcitic marbles. If you start seeing boulangerite, jamesonite, antimonian baumhauerite in float, you are in the right ground. Typical habit: striated, tabular. Train your eye for that shape before scanning the outcrop.




