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, 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.







