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. Macphersonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Macphersonite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals or small clusters of crystals.
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
- 6.64 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals or Small Clusters of Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Lead-zinc Deposits
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find macphersonite
Classic worldwide localities
- Katy Mine, Scotland
- Leadhills, Scotland
- Wanlockhead, Scotland
Field-hunting tip
Look in oxidized hydrothermal lead-zinc deposits country — that is the host setting where macphersonite typically forms. If you start seeing leadhillite, susannite, cerussite in float, you are in the right ground. Field specimens usually show a tabular crystals or small clusters of crystals habit, so train your eye for that shape before scanning the outcrop.





