Leadhillite is a beautiful, rare lead carbonate-sulfate mineral often found in the oxidized zones of lead ore deposits. It is best known for its pseudo-hexagonal crystal habit and its distinct fluorescence, appearing bright yellow or orange under shortwave UV light.
Is this leadhillite?
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 leadhillite with a known reference. Leadhillite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Leadhillite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Leadhillite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow, pale gray, pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: pseudo-hexagonal tabular or rhombohedral crystals.
Often confused with
Leadhillite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside leadhillite
Minerals reported to co-occur with leadhillite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₄SO₄(CO₃)₂(OH)₂
- Mohs hardness
- 2.5
- Density
- 6.55 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Pseudo-hexagonal Tabular or Rhombohedral Crystals
- Cleavage
- Perfect Basal
- Fluorescence
- Bright Yellow to Orange Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead Deposits
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find leadhillite
Classic worldwide localities
- Leadhills, Scotland
- Tiger Mine, Arizona, USA
- Mammoth-St. Anthony Mine, Arizona, USA
- Tsumeb Mine, Namibia
- Broken Hill, Australia
Field-hunting tip
Look in oxidized lead deposits country — that is the host setting where leadhillite typically forms. If you start seeing cerussite, anglesite, pyromorphite in float, you are in the right ground. Field specimens usually show a pseudo-hexagonal tabular or rhombohedral crystals habit, so train your eye for that shape before scanning the outcrop.







