Kegelite is a very rare lead-aluminum silicate sulfate primarily known from the Tsumeb mine in Namibia. It typically occurs as small, pearly-white micaceous plates or crusts in oxidized zones of lead-rich ore bodies.
Is this kegelite?
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 kegelite with a known reference. Kegelite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, pearl white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, micaceous aggregates.
Often confused with
Kegelite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kegelite
Minerals reported to co-occur with kegelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₄Al₂Si₄O₁₀(SO₄)(CO₃)₂(OH)₄
- Mohs hardness
- 2.5
- Density
- 4.46-4.549 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, micaceous aggregates
- Cleavage
- {100}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a deep oxidation zone in a polymetallic mineral deposit
Where rockhounds find kegelite
Classic worldwide localities
- Tsumeb, Namibia
Field-hunting tip
Where it forms: In a deep oxidation zone in a polymetallic mineral deposit. If you start seeing quartz, galena, mimetite in float, you are in the right ground. Typical habit: platy crystals, micaceous aggregates. Train your eye for that shape before scanning the outcrop.








