Carrollite is a rare copper-cobalt sulfide that typically forms distinct, metallic octahedral crystals. Collectors prize it for its bright luster and classic isometric crystal habits found primarily in the Copperbelt region of the Congo.

Hardness
4.5-5.5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this carrollite?

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 carrollite with a known reference. Carrollite sits at Mohs 4.5-5.5, 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: gray, copper red, light gray, steel.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: octahedral crystals, often with curved faces, or massive.

Often confused with

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

Often found alongside carrollite

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

All properties

Chemical formula
CuCo₂S₄
Mohs hardness
4.5-5.5
Density
4.5-4.8 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Cubic
Crystal habit
Octahedral crystals, often with curved faces, or massive
Cleavage
{001}, imperfect
Rarity
Rare
Uses
Collector
Host rock
In hydrothermal vein deposits

Where rockhounds find carrollite

Classic worldwide localities

  • Carroll Co., Maryland, in the Patapsco mine, Finksburg (type locality), and the Mineral Hill mine, Sykesville, USA
  • Boleo, Baja California, Mexico
  • Carrizal Alto copper district, Atacama, Chile
  • Chernomorets, Burgas, Bulgaria
  • Vysna Boca, Nizke Tatry Mountains, Slovakia
  • Kohlenbach mine, near Eiserfeld, and throughout the Siegerland district, North Rhine-Westphalia, Germany

Field-hunting tip

Where it forms: In hydrothermal vein deposits. If you start seeing tetrahedrite, linnaeite, siegenite in float, you are in the right ground. Typical habit: octahedral crystals, often with curved faces, or massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify carrollite?+
Mohs hardness is 4.5-5.5. Luster: metallic. The streak is black. Common colors include gray, copper red, light gray, steel.
Where is carrollite found?+
Notable localities include Carroll Co., Maryland, in the Patapsco mine, Finksburg (type locality), and the Mineral Hill mine, Sykesville, USA; Boleo, Baja California, Mexico; Carrizal Alto copper district, Atacama, Chile; Chernomorets, Burgas, Bulgaria; Vysna Boca, Nizke Tatry Mountains, Slovakia.
Is carrollite safe to handle?+
Carrollite contains cobalt and copper. Contains cobalt and sulfur; avoid creating dust while cleaning or trimming specimens and wash hands thoroughly after handling.
What rocks look like carrollite?+
Carrollite is most often confused with Linnaeite, Siegenite, Pyrite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with carrollite?+
Carrollite commonly co-occurs with Tetrahedrite, Linnaeite, Siegenite, Polydymite, Chalcopyrite, Bornite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does carrollite form in?+
Where it forms: In hydrothermal vein deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is carrollite used for?+
Carrollite is used in collector.

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