Scotlandite is a rare lead sulfite mineral named after its type locality in Leadhills, Scotland. It typically forms thin, transparent, tabular crystals or crusts within the oxidation zones of lead ore deposits. Due to its solubility and rarity, it is highly prized by collectors of lead-species minerals.
Is this scotlandite?
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 scotlandite with a known reference. Scotlandite 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. Scotlandite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Scotlandite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, platy aggregates.
Often confused with
Scotlandite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside scotlandite
Minerals reported to co-occur with scotlandite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbSO₃
- Mohs hardness
- 2-2.5
- Density
- 6.8 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Platy Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Lead-bearing Hydrothermal Veins
- Typical price
- $100-500 per specimen
Where rockhounds find scotlandite
Classic worldwide localities
- Leadhills, Scotland
- Grand Reef Mine, Arizona
- Mina Esperanza, Argentina
Field-hunting tip
Look in oxidized zones of lead-bearing hydrothermal veins country — that is the host setting where scotlandite typically forms. If you start seeing galena, anglesite, cerussite in float, you are in the right ground. Field specimens usually show a tabular crystals, platy aggregates habit, so train your eye for that shape before scanning the outcrop.




