Sulphotsumoite is a rare bismuth telluride sulfide that typically appears as metallic, silver-gray foliated masses or lamellar grains. It is most frequently found in hydrothermal gold-bearing deposits and is often visually indistinguishable from other members of the tetradymite group without X-ray diffraction analysis.

Hardness
2.5
Mohs
Luster
Metallic
Streak
Gray
Transparency
Opaque

Is this sulphotsumoite?

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 sulphotsumoite with a known reference. Sulphotsumoite 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. Streak: 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: gray white.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: aggregates, massive.

Often confused with

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

Often found alongside sulphotsumoite

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

All properties

Chemical formula
Bi₃Te₂S
Mohs hardness
2.5
Density
8.13 g/cm³
Streak
Gray
Luster
Metallic
Transparency
Opaque
Crystal system
Trigonal
Crystal habit
Aggregates, massive
Cleavage
Very perfect in one direction
Rarity
Rare
Uses
Collector
Host rock
Of hydrothermal origin, with other bismuth tellurides

Where rockhounds find sulphotsumoite

Classic worldwide localities

  • Pogo Au–As–Bi–Te deposit, 145 km east of Fairbanks, Alaska, USA
  • Burgagylkan Au–Ag deposit, upper Chelomzha River, Magadan district (type locality), and the Egerlyakh deposit, Indigirka River basin, northeastern Sakha (type locality), Russia
  • Kochbulak gold deposit, Chatkal-Kuramin Mountains, eastern Uzbekistan

Field-hunting tip

Where it forms: Of hydrothermal origin, with other bismuth tellurides. If you start seeing tsumoite, joséite-b in float, you are in the right ground. Typical habit: aggregates, massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify sulphotsumoite?+
Mohs hardness is 2.5. Luster: metallic. The streak is gray. Common colors include gray white.
Where is sulphotsumoite found?+
Notable localities include Pogo Au–As–Bi–Te deposit, 145 km east of Fairbanks, Alaska, USA; Burgagylkan Au–Ag deposit, upper Chelomzha River, Magadan district (type locality), and the Egerlyakh deposit, Indigirka River basin, northeastern Sakha (type locality), Russia; Kochbulak gold deposit, Chatkal-Kuramin Mountains, eastern Uzbekistan.
What rocks look like sulphotsumoite?+
Sulphotsumoite is most often confused with Tetradymite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with sulphotsumoite?+
Sulphotsumoite commonly co-occurs with Tsumoite, Joséite-B. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does sulphotsumoite form in?+
Where it forms: Of hydrothermal origin, with other bismuth tellurides. Working float back to the host body is the standard way to chase a fresh occurrence.
What is sulphotsumoite used for?+
Sulphotsumoite is used in collector.

Find sulphotsumoite on the map

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