Crookesite is an exceptionally rare copper-thallium-silver selenide mineral typically found as small, lead-gray metallic grains in hydrothermal deposits. Collectors prize it primarily for its historical significance in the discovery of the element thallium and its inclusion in rare-earth selenide assemblages. It is almost exclusively found in association with other selenide minerals and requires careful handling due to its toxic chemical composition.

Hardness
2.5-3
Mohs
Luster
Metallic
Streak
Lead-gray
Transparency
Opaque

Is this crookesite?

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 crookesite with a known reference. Crookesite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: 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: blue gray, brown pink, gray.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: disseminated.

Often confused with

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

Often found alongside crookesite

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

All properties

Chemical formula
Cu₇TlSe₄
Mohs hardness
2.5-3
Density
6.90 g/cm³
Colors
Blue grayBrown pinkGray
Streak
Lead-gray
Luster
Metallic
Transparency
Opaque
Crystal system
Tetragonal
Crystal habit
Disseminated
Cleavage
Two at right angles, fairly well developed
Rarity
Rare
Uses
Collector, Scientific research
Host rock
Of hydrothermal origin, with other selenides

Where rockhounds find crookesite

Classic worldwide localities

  • Skrikerum, near Tryserum, Kalmar, Sweden (type locality)
  • Tilkerode, Harz Mountains, Germany
  • Bukov, near Tisnova, and in the Petrovice uranium deposit, near Ždǎr, Czech Republic
  • Pinky Fault uranium deposit, near Lake Athabasca, Saskatchewan, Canada
  • Tuminico, Sierra de Cacho, La Rioja Province, Argentina

Field-hunting tip

Where it forms: Of hydrothermal origin, with other selenides. If you start seeing umangite, berzelianite, eucairite in float, you are in the right ground. Typical habit: disseminated. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify crookesite?+
Mohs hardness is 2.5-3. Luster: metallic. The streak is lead-gray. Common colors include blue gray, brown pink, gray.
Where is crookesite found?+
Notable localities include Skrikerum, near Tryserum, Kalmar, Sweden (type locality); Tilkerode, Harz Mountains, Germany; Bukov, near Tisnova, and in the Petrovice uranium deposit, near Ždǎr, Czech Republic; Pinky Fault uranium deposit, near Lake Athabasca, Saskatchewan, Canada; Tuminico, Sierra de Cacho, La Rioja Province, Argentina.
Is crookesite safe to handle?+
Crookesite contains copper, selenium and thallium and calls for real care. Contains thallium and selenium, both of which are highly toxic. Handle with caution, use protective gear, and wash hands thoroughly after contact.
What rocks look like crookesite?+
Crookesite is most often confused with Eucairite, Berzelianite, Clausthalite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with crookesite?+
Crookesite commonly co-occurs with Umangite, Berzelianite, Eucairite, Klockmannite, Clausthalite, Sabatierite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does crookesite form in?+
Where it forms: Of hydrothermal origin, with other selenides. Working float back to the host body is the standard way to chase a fresh occurrence.
What is crookesite used for?+
Crookesite is used in collector, scientific research.

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