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 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Damaraite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Damaraite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, radiating aggregates.
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
- 2.5
- Density
- 6.68 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Radiating Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Lead-zinc Deposits
- Typical price
- $100-500 per specimen
Where rockhounds find damaraite
Classic worldwide localities
- Tsumeb Mine, Namibia
Field-hunting tip
Look in oxidized hydrothermal lead-zinc deposits country — that is the host setting where damaraite typically forms. If you start seeing galena, cerussite, anglesite in float, you are in the right ground. Field specimens usually show a tabular crystals, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.






