Macphersonite is a rare lead sulfate-carbonate mineral typically found in the oxidation zones of lead deposits. It is most famously identified from the Leadhills-Wanlockhead district in Scotland, where it forms small, delicate crystals often associated with leadhillite and susannite.
Is this macphersonite?
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 macphersonite with a known reference. Macphersonite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine to resinous.
- 4Match the color rangeCompare against the expected color range: white, pale amber brown, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: pseudo hexagonal, tabular.
Often confused with
Macphersonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside macphersonite
Minerals reported to co-occur with macphersonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₄(SO₄)(CO₃)₂(OH)₂
- Mohs hardness
- 2.5-3
- Density
- 6.50-6.55 g/cm³
- Streak
- White
- Luster
- Adamantine to resinous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Pseudo hexagonal, tabular
- Cleavage
- On {010}, perfect
- Fluorescence
- Strong yellow under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An uncommon secondary mineral in the zone of oxidation of lead deposits
Where rockhounds find macphersonite
Classic worldwide localities
- Moon Anchor mine, Maricopa Co., Arizona, USA
- Argentolle mine, near Saint-Prix, Saône-et-Loire, France
- Leadhills, Lanarkshire, Scotland
- Red Gill mine, Caldbeck Fells, Cumbria, England
- Churfürst Ernst mine, Bönkhausen, North Rhine-Westphalia, Germany
- Laurium, Greece, in slag
Field-hunting tip
Where it forms: An uncommon secondary mineral in the zone of oxidation of lead deposits. If you start seeing leadhillite, susannite, cerussite in float, you are in the right ground. Typical habit: pseudo hexagonal, tabular. Train your eye for that shape before scanning the outcrop.





