Damaraite is a very rare lead oxychloride mineral primarily known from the Tsumeb Mine in Namibia. It typically occurs as small, colorless to white tabular crystals or radiating sprays found in the oxidized zones of lead-rich ore bodies.
Is this damaraite?
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 damaraite with a known reference. Damaraite sits at Mohs ~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.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: subhedral crystals.
Often confused with
Damaraite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside damaraite
Minerals reported to co-occur with damaraite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃O₂(OH)Cl
- Mohs hardness
- ~3
- Density
- 7.84 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Subhedral crystals
- Cleavage
- {010}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- From a late-stage vein cutting a banded manganese ore lens in Cu–Pb–Ag ores formed by hydrothermal and metasomatic replacement of dolostones (Kombat mine, Namibia)
Where rockhounds find damaraite
Classic worldwide localities
- Kombat Cu–Pb–Ag mine, 49 km south of Tsumeb, Namibia
- Laurium, Greece, in slag
- Found in the Elura Zn–Pb–Ag deposit, 43 km northeast of Cobar, New South Wales, Australia
Field-hunting tip
Where it forms: From a late-stage vein cutting a banded manganese ore lens in Cu–Pb–Ag ores formed by hydrothermal and metasomatic replacement of dolostones (Kombat mine, Namibia). If you start seeing jacobsite, hausmannite, hematophanite in float, you are in the right ground. Typical habit: subhedral crystals. Train your eye for that shape before scanning the outcrop.








