Dugganite is a rare lead zinc tellurate arsenate mineral typically found as small, green, hexagonal prismatic crystals or crusts. It is most famous for its occurrence in the oxidized zones of the mines in Tombstone, Arizona, where it appears alongside other rare secondary minerals. Due to its arsenic and lead content, collectors should handle specimens with care and store them securely.
Is this dugganite?
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 dugganite with a known reference. Dugganite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dugganite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Dugganite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellow-green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: hexagonal prisms, crusts, coatings.
Often confused with
Dugganite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside dugganite
Minerals reported to co-occur with dugganite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃Zn₃(Te⁶⁺O₆)(AsO₄)₂
- Mohs hardness
- 3.5
- Density
- 5.65 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Hexagonal Prisms, Crusts, Coatings
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find dugganite
Classic worldwide localities
- Tombstone, Arizona, USA
Field-hunting tip
Look in oxidized hydrothermal veins country — that is the host setting where dugganite typically forms. If you start seeing quartz, mimetite, wulfenite in float, you are in the right ground. Field specimens usually show a hexagonal prisms, crusts, coatings habit, so train your eye for that shape before scanning the outcrop.




