Padĕraite is an extremely rare sulfosalt mineral primarily found in hydrothermal veins. It typically presents as metallic, steel-gray grains or small aggregates embedded within other sulfide ores, making it a prized specimen for advanced collectors of complex bismuth-lead minerals.

Hardness
4
Mohs
Luster
Metallic
Streak
Lead gray
Transparency
Opaque

Is this padĕraite?

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 padĕraite with a known reference. Padĕraite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: lead gray.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: steel gray, black.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: fibrous, platy.

Often confused with

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

Often found alongside padĕraite

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

All properties

Chemical formula
Cu₇(Cu,Ag)₀.₃₃Pb₁.₃₃Bi₁₁.₃₃S₂₂
Mohs hardness
4
Density
6.91 g/cm³
Streak
Lead gray
Luster
Metallic
Transparency
Opaque
Crystal system
Monoclinic
Crystal habit
Fibrous, platy
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Intimately intergrown with other Pb-Bi sulfosalts, particularly, members of the cuprobismutite series and the bismuthinite-aikinite homologous series

Where rockhounds find padĕraite

Classic worldwide localities

  • Romania, from Băiţa (Rézbánya) (type locality), and in the Paulus mine, Ocna de Fier (Morávicza, Vaskő)
  • Banská Stiavnica (Schemnitz), Slovakia
  • Swartberg, northern Cape Province, South Africa

Field-hunting tip

Where it forms: Intimately intergrown with other Pb-Bi sulfosalts, particularly, members of the cuprobismutite series and the bismuthinite-aikinite homologous series. If you start seeing hammarite, pekoite, bismuthinite in float, you are in the right ground. Typical habit: fibrous, platy. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify padĕraite?+
Mohs hardness is 4. Luster: metallic. The streak is lead gray. Common colors include steel gray, black.
Where is padĕraite found?+
Notable localities include Romania, from Băiţa (Rézbánya) (type locality), and in the Paulus mine, Ocna de Fier (Morávicza, Vaskő); Banská Stiavnica (Schemnitz), Slovakia; Swartberg, northern Cape Province, South Africa.
Is padĕraite safe to handle?+
Padĕraite contains copper and lead. Contains lead and bismuth; handle with care and wash hands thoroughly after handling. Do not ingest or inhale dust.
What rocks look like padĕraite?+
Padĕraite is most often confused with Galena, Wittichenite, Bismuthinite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with padĕraite?+
Padĕraite commonly co-occurs with Hammarite, Pekoite, Bismuthinite, Cuprobismutite, Hodrushite, Chalcopyrite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does padĕraite form in?+
Where it forms: Intimately intergrown with other Pb-Bi sulfosalts, particularly, members of the cuprobismutite series and the bismuthinite-aikinite homologous series. Working float back to the host body is the standard way to chase a fresh occurrence.
What is padĕraite used for?+
Padĕraite is used in collector.

Find padĕraite on the map

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