Itoite is a rare lead germanium mineral primarily found in the oxidized zones of lead-rich ore deposits. It typically forms delicate tabular crystals or thin plates that are often confused with more common lead carbonates like cerussite. Collectors prize it for its association with the unique mineralogy of the Tsumeb mine in Namibia.
Is this itoite?
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 itoite with a known reference. Itoite 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. Itoite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Itoite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, thin plates, aggregates.
Often confused with
Itoite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside itoite
Minerals reported to co-occur with itoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃GeO₂(OH)₄
- Mohs hardness
- 2.5
- Density
- 6.35 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Thin Plates, Aggregates
- Cleavage
- Distinct On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Lead-germanium Ore Deposits
- Typical price
- $100-500 for small thumbnail specimens
Where rockhounds find itoite
Classic worldwide localities
- Tsumeb Mine, Namibia
Field-hunting tip
Look in oxidized hydrothermal lead-germanium ore deposits country — that is the host setting where itoite typically forms. If you start seeing tsumebite, cerussite, anglesite in float, you are in the right ground. Field specimens usually show a tabular crystals, thin plates, aggregates habit, so train your eye for that shape before scanning the outcrop.




