Pilsenite is a rare bismuth telluride mineral that typically appears as lead-gray to silver-white metallic flakes or tabular crystals. It is most frequently found in hydrothermal gold deposits where it is often associated with other tellurides and sulfides. Collectors should note its perfect basal cleavage and distinct metallic luster, which make it look remarkably similar to other members of the tetradymite group.

Hardness
1.5-2.5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this pilsenite?

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 pilsenite with a known reference. Pilsenite sits at Mohs 1.5-2.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: black.
  • 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, tin white.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: tabular crystals, foliated masses, or disseminated grains.

Often confused with

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

Often found alongside pilsenite

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

All properties

Chemical formula
Bi₄Te₃
Mohs hardness
1.5-2.5
Density
8.41 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Trigonal
Crystal habit
Tabular crystals, foliated masses, or disseminated grains
Cleavage
Perfect
Rarity
Rare
Uses
Collector
Host rock
Of hydrothermal origin

Where rockhounds find pilsenite

Classic worldwide localities

  • Sylvanite, Hidalgo Co., New Mexico, USA
  • Nagybörzsöny, Börzsöny Mountains, near Esztergom (Gran), Hungary (type locality)
  • Săcărı̂mb (Nagyág), Romania
  • Koronuda Au–Cu deposit, Macedonia
  • Bereznyakov gold deposit, Southern Ural Mountains, Russia
  • Corrego Criminosa gold district, Goias, Brazil

Field-hunting tip

Where it forms: Of hydrothermal origin. If you start seeing hessite, joséite, bismuthinite in float, you are in the right ground. Typical habit: tabular crystals, foliated masses, or disseminated grains. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify pilsenite?+
Mohs hardness is 1.5-2.5. Luster: metallic. The streak is black. Common colors include steel gray, tin white.
Where is pilsenite found?+
Notable localities include Sylvanite, Hidalgo Co., New Mexico, USA; Nagybörzsöny, Börzsöny Mountains, near Esztergom (Gran), Hungary (type locality); Săcărı̂mb (Nagyág), Romania; Koronuda Au–Cu deposit, Macedonia; Bereznyakov gold deposit, Southern Ural Mountains, Russia.
Is pilsenite safe to handle?+
Contains bismuth and tellurium; handle with care and avoid dust inhalation or ingestion.
What rocks look like pilsenite?+
Pilsenite is most often confused with Tetradymite, Tellurobismuthite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with pilsenite?+
Pilsenite commonly co-occurs with Hessite, Joséite, Bismuthinite, Tsumoite, Argentian pentlandite, Argentian tetrahedrite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pilsenite form in?+
Where it forms: Of hydrothermal origin. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pilsenite used for?+
Pilsenite is used in collector.

Find pilsenite on the map

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