Carlinite is a rare thallium sulfide mineral typically found as microscopic inclusions within gold-bearing sediment deposits. It is best known as a type-locality mineral from the Carlin trend in Nevada, where it was first identified through electron microprobe analysis. Due to its extreme rarity and toxicity, it is almost exclusively held in research-grade mineral collections.

Hardness
~1
Mohs
Luster
Bright metallic
Streak
Dark gray to black
Transparency
Opaque

Is this carlinite?

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 carlinite with a known reference. Carlinite sits at Mohs ~1, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: dark gray to black.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: bright metallic.
  • 4
    Match the color range
    Compare against the expected color range: dark gray, black.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: microscopic grains, anhedral masses.

Often confused with

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

Often found alongside carlinite

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

All properties

Chemical formula
Tl₂S
Mohs hardness
~1
Density
8.1 g/cm³
Streak
Dark gray to black
Luster
Bright metallic
Transparency
Opaque
Crystal system
Trigonal
Crystal habit
Microscopic grains, anhedral masses
Cleavage
{0001}, perfect, and an imperfect prismatic cleavage
Rarity
Rare
Uses
Collector, Scientific research
Host rock
As small grains in brecciated fragments of carbonaceous limestone, a result of epithermal mineralization

Where rockhounds find carlinite

Classic worldwide localities

  • East pit of the Carlin mine (type locality), 50 km northwest of Elko, and in the Deep Post orebody, Goldstrike mine, Lynn district, Eureka Co., Nevada, USA

Field-hunting tip

Where it forms: As small grains in brecciated fragments of carbonaceous limestone, a result of epithermal mineralization. If you start seeing gold, arsenic, antimony in float, you are in the right ground. Typical habit: microscopic grains, anhedral masses. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify carlinite?+
Mohs hardness is ~1. Luster: bright metallic. The streak is dark gray to black. Common colors include dark gray, black.
Where is carlinite found?+
Notable localities include East pit of the Carlin mine (type locality), 50 km northwest of Elko, and in the Deep Post orebody, Goldstrike mine, Lynn district, Eureka Co., Nevada, USA.
Is carlinite safe to handle?+
Carlinite contains thallium and calls for real care. Carlinite contains thallium, a highly toxic heavy metal. Handle with gloves, wash hands thoroughly after contact, and avoid inhaling dust or vapors; do not ingest.
What rocks look like carlinite?+
Carlinite is most often confused with Orpiment, Realgar, Stibnite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with carlinite?+
Carlinite commonly co-occurs with Gold, Arsenic, Antimony, Mercury, Avicennite, Organic carbon. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does carlinite form in?+
Where it forms: As small grains in brecciated fragments of carbonaceous limestone, a result of epithermal mineralization. Working float back to the host body is the standard way to chase a fresh occurrence.
What is carlinite used for?+
Carlinite is used in collector, scientific research.

Find carlinite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

Download on the App StoreGet it on Google Play