Matlockite is a rare lead halide mineral known for its high refractive index and excellent adamantine luster. It typically forms thin, transparent, tabular crystals in the oxidation zones of lead-bearing ore deposits.
Is this matlockite?
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 matlockite with a known reference. Matlockite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine, pearly on {001}.
- 4Match the color rangeCompare against the expected color range: brownish yellow, colorless, green yellow, dark yellow brown.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: crystalline, tabular.
Often confused with
Matlockite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside matlockite
Minerals reported to co-occur with matlockite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbFCl
- Mohs hardness
- 2.5-3
- Density
- 7.12 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine, pearly on {001}
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Crystalline, tabular
- Cleavage
- {001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxide zone of some lead-bearing mineral deposits
Where rockhounds find matlockite
Classic worldwide localities
- Mammoth-St. Anthony mine, Tiger, Pinal Co., USA
- Apache mine, Gila Co., USA
- Mildren mine, Cabibi district, South Comobabi Mountains, Arizona, USA
- Bage and Wallclose mines, about 2.5 km south of Matlock, Derbyshire, England
- Slag, at Laurium, Greece
- Slag, along Baratti Beach and one km north of Campiglia, Tuscany, Italy
Field-hunting tip
Where it forms: In the oxide zone of some lead-bearing mineral deposits. If you start seeing phosgenite, anglesite, cerussite in float, you are in the right ground. Typical habit: crystalline, tabular. Train your eye for that shape before scanning the outcrop.






