Plumboagardite is a rare secondary mineral found in the oxidized zones of copper-lead deposits. It typically forms as small, attractive emerald-green crystalline crusts or distinct, tiny rhombohedral crystals, most famously from the Tsumeb mine.

Hardness
3
Mohs
Luster
Vitreous
Streak
Greenish
Transparency
Translucent

Is this plumboagardite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch plumboagardite with a known reference. Plumboagardite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: greenish.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: grass green.
  • 5
    Look at form & habit
    Crystal system: hexagonal. Typical habit: aggregates, radial, spherical.

Often confused with

Plumboagardite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside plumboagardite

Minerals reported to co-occur with plumboagardite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
PbCu₆(AsO₄)₂(AsO₃OH)(OH)₆(H₂O)₃
Mohs hardness
3
Density
3.471 g/cm³
Streak
Greenish
Luster
Vitreous
Transparency
Translucent
Crystal system
Hexagonal
Crystal habit
Aggregates, radial, spherical
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Formed in the oxidized zone of hydrothermal Pb-Zn vein deposits, the product of alteration of primary Pb, Cu, REE, and As minerals

Where rockhounds find plumboagardite

Classic worldwide localities

  • Waste dumps of the Aitern-Süd mine, near Schönau, Baden-Württemberg, Germany
  • Miedzianka-Ciechanowice deposits, Rudawy Janowickie Mountains, Lower Silesia, Poland

Field-hunting tip

Where it forms: Formed in the oxidized zone of hydrothermal Pb-Zn vein deposits, the product of alteration of primary Pb, Cu, REE, and As minerals. If you start seeing fluorite, limonite, chrysocolla in float, you are in the right ground. Typical habit: aggregates, radial, spherical. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify plumboagardite?+
Mohs hardness is 3. Luster: vitreous. The streak is greenish. Common colors include grass green.
Where is plumboagardite found?+
Notable localities include Waste dumps of the Aitern-Süd mine, near Schönau, Baden-Württemberg, Germany; Miedzianka-Ciechanowice deposits, Rudawy Janowickie Mountains, Lower Silesia, Poland.
Is plumboagardite safe to handle?+
Plumboagardite contains arsenic, copper and lead and calls for real care. Contains arsenic and lead; handle with care and wash hands thoroughly after handling. Do not inhale dust or allow to be ingested.
What rocks look like plumboagardite?+
Plumboagardite is most often confused with Mixite, Corkite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with plumboagardite?+
Plumboagardite commonly co-occurs with Fluorite, Limonite, Chrysocolla, Quartz. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does plumboagardite form in?+
Where it forms: Formed in the oxidized zone of hydrothermal Pb-Zn vein deposits, the product of alteration of primary Pb, Cu, REE, and As minerals. Working float back to the host body is the standard way to chase a fresh occurrence.
What is plumboagardite used for?+
Plumboagardite is used in collector.

Find plumboagardite on the map

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