Mattheddleite is a rare lead silicate-sulfate mineral named after the Scottish mineralogist Matthew Forster Heddle. It typically appears as small, colorless to pale yellow prismatic crystals found in the oxidized zones of lead-zinc mines, specifically in the Leadhills-Wanlockhead district of Scotland.
Is this mattheddleite?
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 mattheddleite with a known reference. Mattheddleite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mattheddleite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mattheddleite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Mattheddleite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mattheddleite
Minerals reported to co-occur with mattheddleite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂₀(SiO₄)₇(SO₄)₄Cl₄
- Mohs hardness
- 3.5
- Density
- 4.62 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Lead-zinc Deposits
- Typical price
- $50-300+ per specimen depending on crystal size
Where rockhounds find mattheddleite
Classic worldwide localities
- Leadhills, Scotland
- Wanlockhead, Scotland
Field-hunting tip
Look in oxidized hydrothermal lead-zinc deposits country — that is the host setting where mattheddleite typically forms. If you start seeing cerussite, galena, anglesite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





