Lanarkite is a rare lead sulfate mineral primarily found in the oxidized zones of lead mines. It is best known for its high-luster, bladed crystals that typically occur in small, delicate clusters often associated with other lead minerals like anglesite and cerussite.
Is this lanarkite?
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 lanarkite with a known reference. Lanarkite sits at Mohs 2-2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Lanarkite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lanarkite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish-white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: lath-like, tabular crystals, sometimes bladed or massive.
Often confused with
Lanarkite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lanarkite
Minerals reported to co-occur with lanarkite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂OSO₄
- Mohs hardness
- 2-2.5
- Density
- 6.8-6.9 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Lath-like, Tabular Crystals, Sometimes Bladed or Massive
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Lead-bearing Hydrothermal Veins
- Typical price
- $50-500 thumbnail
Where rockhounds find lanarkite
Classic worldwide localities
- Leadhills, Scotland
- Red Cloud Mine, Arizona, USA
- Mammoth-Saint Anthony Mine, Arizona, USA
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized zones of lead-bearing hydrothermal veins country — that is the host setting where lanarkite typically forms. If you start seeing anglesite, cerussite, galena in float, you are in the right ground. Field specimens usually show a lath-like, tabular crystals, sometimes bladed or massive habit, so train your eye for that shape before scanning the outcrop.




