Dundasite is an attractive secondary lead mineral that typically forms delicate, snowy-white or pale-colored radiating spherical clusters. It is highly sought after by collectors for its aesthetic, pom-pom like habits, particularly when found associated with brilliant orange Crocoite.
Is this dundasite?
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 dundasite with a known reference. Dundasite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dundasite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Dundasite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow, pale green, blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: spherical aggregates, radiating sprays, crusts, botryoidal.
Often confused with
Dundasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside dundasite
Minerals reported to co-occur with dundasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbAl₂(CO₃)₂(OH)₄·2H₂O
- Mohs hardness
- 3.5-4
- Density
- 3.2-3.3 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Spherical Aggregates, Radiating Sprays, Crusts, Botryoidal
- Cleavage
- Perfect
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Oxidized Lead Deposits
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find dundasite
Classic worldwide localities
- Dundas, Tasmania
- Tsumeb, Namibia
- Touissit, Morocco
- Arizona, USA
Field-hunting tip
Look in oxidized lead deposits country — that is the host setting where dundasite typically forms. If you start seeing cerussite, crocoite, gibbsite in float, you are in the right ground. Field specimens usually show a spherical aggregates, radiating sprays, crusts, botryoidal habit, so train your eye for that shape before scanning the outcrop.





