Cotunnite is a rare lead chloride mineral typically forming as a sublimation product at volcanic fumaroles or as an oxidation product of galena. Collectors look for its characteristic adamantine luster and thin, colorless to yellowish orthorhombic crystals. Due to its solubility and lead content, it should be kept in a dry display environment and handled with proper care.

Hardness
2.5
Mohs
Luster
Adamantine
Streak
White
Transparency
Transparent

Is this cotunnite?

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 cotunnite with a known reference. Cotunnite sits at Mohs 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. Cotunnite leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Cotunnite typically shows a adamantine luster.
  • 4
    Match the color range
    Compare against the expected color range: white, colorless, yellowish, greenish.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: acicular or prismatic crystals, also found as crystalline crusts or incrustations.

Often confused with

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

Often found alongside cotunnite

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

All properties

Chemical formula
PbCl₂
Mohs hardness
2.5
Density
5.3 g/cm³
Streak
White
Luster
Adamantine
Transparency
Transparent
Crystal system
Orthorhombic
Crystal habit
Acicular or Prismatic Crystals, Also Found as Crystalline Crusts or Incrustations
Cleavage
Perfect On {001}
Rarity
Rare
Uses
Collector
Host rock
Fumaroles and Oxidized Zones of Lead-bearing Ore Deposits
Typical price
$50-500 depending on specimen quality and size

Where rockhounds find cotunnite

Classic worldwide localities

  • Mount Vesuvius, Italy
  • Lavrion District, Greece
  • Tolbachik Volcano, Russia
  • Sierra Gorda, Chile

Field-hunting tip

Look in fumaroles and oxidized zones of lead-bearing ore deposits country — that is the host setting where cotunnite typically forms. If you start seeing galena, anglesite, cerussite in float, you are in the right ground. Field specimens usually show a acicular or prismatic crystals, also found as crystalline crusts or incrustations habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify cotunnite?+
Mohs hardness is 2.5. It typically shows a adamantine luster. The streak is white. Common colors include white, colorless, yellowish, greenish.
Where is cotunnite found?+
Notable localities include Mount Vesuvius, Italy; Lavrion District, Greece; Tolbachik Volcano, Russia; Sierra Gorda, Chile.
How much is cotunnite worth?+
Typical asking prices fall in the range of $50-500 depending on specimen quality and size. Quality, size, and provenance can move individual specimens well outside that range.
Is cotunnite safe to handle?+
It contains toxic constituents. Contains lead, which is toxic if ingested or inhaled as dust; wash hands thoroughly after handling and avoid grinding or creating dust. Handle with care, avoid grinding or breathing dust, and store separately.
What rocks look like cotunnite?+
Cotunnite is most often confused with Anglesite, Cerussite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with cotunnite?+
Cotunnite commonly co-occurs with Galena, Anglesite, Cerussite, Phosgenite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does cotunnite form in?+
Cotunnite typically forms in fumaroles and oxidized zones of lead-bearing ore deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is cotunnite used for?+
Cotunnite is used in collector.

Find cotunnite on the map

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